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Photographic 

Sciences 

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23  WEST  MAIN  STREET 

WEBSTER,  N.Y.  14580 

(716)  872-4503 


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CIHM/ICMH 

Microfiche 

Series. 


CIHM/ICMH 
Collection  de 
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Canadian  Institute  for  Historical  Microreproductions  /  Institut  Canadian  de  microreproductions  historiques 


Technical  and  Bibliographic  Notes/Notes  techniques  et  bibiiographiques 


The  Institute  has  attempted  to  obtain  the  best 
original  copy  available  for  filming.  Features  of  this 
copy  which  may  be  bibliographicaily  unique, 
which  may  alter  any  of  the  images  in  the 
reproduction,  or  which  may  significantly  change 
the  usual  method  of  filming,  are  checked  below. 


D 


D 


D 
0 


D 


n 


Coloured  covers/ 
Couverture  de  couleur 


I     I   Covers  damaged/ 


Couverture  endommagAe 


Covers  restored  and/or  laminated/ 
Couverture  restaurAe  et/ou  pellicula 


pn   Cover  title  missing/ 


Le  titre  de  couverture  manque 

Coloured  maps/ 

Cartes  gAographiques  en  couleur 


□    Coloured  Ink  (i.e.  other  than  blue  or  black)/ 
Encre  de  couleur  (i.e.  autre  que  bleue  ou  noire) 

|~~|   Coloured  plates  and/or  illustrations/ 


Planches  et/ou  illustrations  en  couleur 

Bound  with  other  material/ 
ReilA  avec  d'autres  documents 

Tight  binding  may  cause  shadows  or  distortion 
along  interior  tiargin/ 

La  re  liure  serr^e  peut  causer  de  I'ombre  ou  de  la 
distortion  le  long  de  la  marge  IntArieure 

Blank  leaves  added  during  restoration  may 
appear  within  the  text.  Whenever  possible,  these 
have  been  omitted  from  filming/ 
II  se  peut  que  certaines  pages  blanches  ajout^es 
lors  d'une  restauration  apparaissent  dans  le  texte, 
mais,  lorsque  cela  Atait  possible,  ces  pages  n'ont 
pas  At*  film6es. 

Additional  comments:/ 
Commentaires  supplAmentaires: 


L'Institut  a  microfilm*  le  meilleur  exempiaire 
qu'il  lui  a  *t*  possible  de  se  procurer.  Les  details 
de  cet  exempiaire  qui  sont  peut-Atre  uniques  du 
point  de  vue  bibliographique.  qui  peuvent  modifier 
une  image  reproduite,  ou  qui  peuvent  exiger  une 
modification  dans  la  methods  normaie  de  filmage 
sont  I  idiqute  ci-dessous. 


D 
D 
D 
IZI 
D 
0 
0 
D 
D 
D 


This  item  is  filmed  at  the  reduction  ratio  checked  iselow/ 

Ce  document  est  film*  au  taux  de  roojction  indiquA  ci-dessous. 


Coloured  pages/ 
Pages  de  couleur 

Pages  damaged/ 
Pages  endommagtes 

Pages  restored  and/or  laminated/ 
Pages  restaur^es  et/ou  pellicultes 

Pages  discoloured,  stained  or  foxed/ 
Pages  dteolortes,  tachettes  ou  piqutes 

Pages  detached/ 
Pages  ditachtos 

Showthrough/ 
Transparence 

Quality  of  print  varies/ 
Quality  inAgale  de  I'impression 

Includes  supplementary  material/ 
Comprend  du  mat6riel  supplAmentaire 

Only  edition  available/ 
Seule  Edition  disponible 

Pages  wholly  or  partially  obscured  by  errata 
slips,  tissues,  etc.,  have  been  refilmed  to 
ensure  the  best  possible  image/ 
Les  pages  totaiement  ou  partiellement 
obscurcies  par  un  feuillet  d'errata,  une  pelure, 
etc.,  ont  At*  filmAes  A  nouveau  de  fapon  A 
obtenir  la  meilleure  image  possible. 


10X 

14X 

18X 

22X 

26X 

30X 

I 

12X 

16X 

aox 

24X 

28X 

32X 

aire 

details 
uas  du 
t  modifier 
gar  una 

filmaga 


Tha  copy  filmad  hara  has  baan  rsproducad  thanks 
to  tha  ganarosity  of: 

Thomas  Fiihar  Rara  Book  Library, 
Univanity  of  Toronto  Library 

Tha  images  appearing  hare  are  the  best  quaiity 
possible  considering  the  condition  and  (agibility 
of  the  original  copy  and  in  keeping  with  the 
filming  contract  specifications. 


Original  copies  in  printed  paper  covers  are  filmed 
beginning  with  the  front  cover  and  ending  on 
the  last  page  with  a  printed  or  illustreted  impres- 
sion, or  the  back  cover  when  appropriate.  All 
other  original  copies  are  filmed  beginning  on  the 
first  page  with  a  printed  or  illustrated  impres- 
sion, and  ending  on  the  last  page  with  a  printed 
or  illustrated  impression. 


/ 
utes 


L'exemplaire  film*  fut  reproduit  grice  k  la 
ginirosit*  de: 

Thomas  Fishar  Rara  Book  Library, 
Univarsity  of  Toronto  Library 

Les  images  suivantes  ont  ^t(t  reproduites  avec  la 
plus  grand  soin,  compte  tenu  de  la  condition  et 
de  la  nettet«  de  l'exemplaire  film*,  et  en 
conformity  avec  les  conditions  du  contrat  de 
filmaga. 

Les  exemplaires  originaux  dont  la  couvertiire  en 
papier  est  imprimie  sont  filmis  en  commenpant 
par  la  premier  plat  et  en  terminant  soit  par  la 
darniire  page  qui  comporte  une  empreinte 
d'impression  ou  d'iilustration.  soit  par  le  second 
plat,  salon  le  cas.  Tous  les  autres  exemplaires 
originaux  sont  filmAs  en  commenpant  par  la 
premiere  page  qui  comporte  une  empreinte 
d'impression  ou  d'iiiustration  et  en  terminant  par 
la  darniire  page  qui  comporte  une  telle 
empreinte. 


The  last  recorded  freme  on  eech  microfiche 
shell  contain  the  symbol  — ^>  (meening  "CON- 
TINUED"), or  the  symbol  y  (meaning  "END"), 
whichever  epplies. 


Un  des  symboles  suivants  apparaitra  sur  la 
darniire  image  de  cheque  microfiche,  selon  le 
CBs:  le  symbols  — »•  signifie  "A  SUIVRE",  le 
symbols  V  signifie  "FIN '. 


lire 


Maps,  plates,  charts,  etc.,  may  be  filmed  et 
different  reduction  ratios.  Those  too  lerge  to  be 
entirely  included  in  one  exposure  ere  filmed 
beginning  in  the  upper  left  hend  corner,  left  to 
right  and  top  to  bottom,  as  many  frames  as 
required.  The  following  diograms  illustrate  the 
method: 


Les  certes,  planches,  tableaux,  etc.,  peuvent  Atre 
filmis  i  des  taux  de  rMuction  diff brents. 
Lorsque  ie  document  est  trop  grand  pour  dtre 
reproduit  en  un  seul  clich6,  il  est  f  iimA  A  partir 
de  I'engie  supirieur  gauche,  de  gauche  d  droite, 
et  de  heut  en  bes,  en  prenant  le  nombre 
d'imeges  n6cessaire.  Les  diagrammes  suivants 
illustrent  la  mithode. 


by  errata 
led  to 

Bnt 

me  pelure, 

apon  d 


1  2  3 


32X 


1 

2 

3 

4 

5 

6 

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^  THE 

POSSIBILITY 

«p 

APPROACHING  THE  NORTH  POLE 

ASSERTED. 


t  BY 


?«• 


THE  HOX.  B^'MRRIJ^GTOX. 

A  NEW  EDITION. 

WITH 

AN  APPENDIX, 

CONTAINING 

PAPERS  ON  THE  SAME  SUBJECT, 


BT 


C0L03^Eh   BEAUFOr,    F.B,S. 

ILLUSTRATED   WITH   A   MAP  OF    THE   NORTH   POLE,   ACCORDING 
TO   THE   LATEST   DISCOVERIES. 


jj^eto-'JIatli: 


PUBLISHED  BY  JAMES  EASTBVRN  ic  CO. 
AT  THE  LITERARY  ROOMS,  BROADWAY,  CORNER  OF  FINE-STREET.. 


V^t, 


ABRAHAM   PAUL,   PRINTIR. 

1818. 


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-'■.,       4'  *:"     ''     ■   ' 

•  "i^  '■•../,' ;.-., 

■■   ',>i  [.    ff*'  '     .' 

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,•     t- 

PBEFAC?:. 

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— ««WW— 


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ur» 


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■  } 

i 


XHE  interesting  nature  of  the  sml^et  to  which  the 
fpUowiog  Paperis  relate,  would,  at  any  time,  justify 
their  republication;  hut  fit  the  present  moqnent  they 
derive  an  additional  value  trcmi  the  eKpeditioii  which 
19  mow  preparing  to  ei^plore  the  Arctic  I^egions. 
Whether  the  ei^tended  boundaries  of  geographical 
8cieoce»  tided  by  the  local  inforniation  which  it  is 
aaid  hai9  been  c(»nmunicated  by  those  who  are  em- 
ployed in  the  Crreenland  Fisheries,  will  secure  the 
success  of  this  enterprise,  it  is  impossible  to  antici- 
pate; but;  as  Englishmen,  we  must  naturally  wish; 
tbai  diseoveries,  which  were  first  attempted  by  the 
lidventurous  spirit  and  maritime  skill  of  our  country- 
nieQ,  should  be  finally  achieved  by  the  same  means. 

As  early  as  the  year  1527,  the  idea  of  a  passage  •to 
Ihe  jB^st  Indies  by  the  North  Pole  was  suggested  by 
a  Bristol  Merchant  to  Henry  VIII;  but  no  voyage 
seen^i  to  have  been  undertaken  for  the  purpose  of 


ir 


PRGFAClS. 


navigating  the  Circumpolar  Seas  till  the  commence- 
ment of  the  following  century,  when,  in  1607,  an  ex- 
pedition was  fitted  out,  at  the  expense  of  certain  Mer- 
chants of  London.  To  this  attempt  several  others 
succeeded  at  different  periods,  and  all  of  them  were 
projected  and  carried  into  execution  hy  private  indi- 
viduals. The  adventurers  did  not  indeed  accomplish 
the  object  they  exclusively  sought,  that  of  reaching 
India  by  a  nearer  route  than  doubling  the  Cape  of 
Good  Hope ;  but  though  they  failed  in  that  respect, 
the  fortitude,  perseverance,  and  skill  which  they  mani- 
fested, exhibited  the  most  irrefragable  proofs  of  the 
early  existence  of  that  superiority  in  naval  afiairs, 
which  has  progressively  elevated  this  country  to  her 
present  eminence  among  the  nations  of  Europe.  -  >  > '  ^ 
''  At  length,  after  the  lapse  of  above  a  century  and  a 
half,  this  interesting  question  became  an  object  of 
royal  patronage,  and  the  expedition  which  was  com- 
manded by  Captain  Phipps,  afterward  Lord  Mul- 
grave,  in  1773,  was  fitted  out  at  the  charge  of  Go- 
vernment. It  will  add  to  the  value  of  the  following 
pages  when  it  is  known,  that  the  author  of  them  was 
*he  first  proposer  of  this  memorable  voyage ;  and  that 
in*consequence  of  his  representations,  as  to  the  prac- 
ticability of  circumnavigating  the  Pole,  the  Royal  So- 
ciety made  their  application  to  Lord  Sandwich,  then 
at  the  head  of  the  Admiralty,    which  led  to  the 


appomti 
p'»gion8. 

Thouj 
traf  e  the 
twenty  d 
the  opin 
of  proce 
remained 
therefore 
with  the 
rials  he  i 
of  writte 
afterwart 
be  denie 
is  at  leaE 
value  wl 
so  acute 

The 
mitted 
ing,  as 
subject 
of  that 
reachini 
winter, 
drawn 
ous  quel 


PRRfACE. 


ommence- 

07,  an  ex- 

rtain  Mer- 

ral  others 

them  were 

rivate  indi- 

Eiccomplish 

)f  reaching 

le  Cape  of 

lat  respect, 

I  they  mani- 

oofs  of  the 

ival  affairs, 

ntry  to  her 

rope. 

»ntury  and  a 
n  object  of 
;h  was  corn- 
Lord  Mul- 
irge  of  Go- 
\e  following 
>f  them  was 
;e ;  and  that 
to  the  prac- 
le  Royal  So- 
dwich,  then 
led  to  the 


i 


appomtment  of  the  expedition  for  exploring  those 

Though  Captain  Phipps  found  it  impossible  to  pene- 
trate the  wall  of  ice,  which  extended  for  more  than 
twenty  degrees  between  the  latitudes  of  80**  and  81^ 
the  opinions  of  Mr.  Barrington  upon  the  possibility 
of  proceeding  farther,  under  different  circumstances, 
remained  unshaken.  With  indefatigable  assiduity 
therefore  he  began  to  collect  every  fact  connected 
with  the  subject ;  and  as  he  accumulated  liis  mate- 
rials he  read  them  to  the  Royal  Society.  This  mass 
of  written,  traditionary,  and  conjectural  evidence,  he 
afterward  published,  in  the  year  1775;  and  it  cannot 
be  denied  that  its  republication  at  the  present  moment 
is  at  least  appropriate,  independently  of  the  Intrinsic 
value  which  must  always  attach  to  the  researches  of 
so  acute  and  ardent  an  inquirer.  it^>  -ra^^  ~^».n 

The  Publishers,  however,  are  happy  in  being  per- 
mitted to  add  to  the  value  of  these  Tracts,  by  subjoin- 
ing, as  an  Appendix,  some  Papers  upon  the  same 
subject  by  Colonel  Beaufoy,  F.  R.  S.  The  attention 
of  that  gentleman  was  turned  to  the  practicability  of 
reaching  the  North  Pole,  from  Spitzbergen,  during 
winter,  by  travelling  over  the  ice  and  snow  in  sledges 
drawn  by  rein  deer.  He  therefore  transmitted  vari- 
ous queries,  to  which  he  received  answers  from  Rus- 


fl 


rRKVACV. 


m 


4 


■iani  who  bad  wintered  in  those  remote  islands.  The 
information  thus  elicited  is  exceedingly  curious,  and 
much  of  it  may  be  most  advantageously  employed  by 
those  who  are  about  to  brave  the  dangers  and  incle- 
mencies of  that  dreary  climate.        .1 

In  order  to  render  the  present  volume  as  complete 
AS  possible,  an  entirely  new  Map  of  the  North  Pole 
is  prefixed,  drawn  from  the  best  authorities,  and  with 
the  Pole  in  the  centre,  so  as  to  exhibit  the  utmost  de- 
gree of  latitude  which  has  hitherto  been  approached. 
Under  all  these  circumstances,  it  is  hoped  (he  Woric 
will  find  a  fitvourable  reception.  Its  claims,  indeed, 
are  of  no  dubious  nature ;  for  it  b  the  production  of 
persons  eminent  for  their  scientific  attainments.  Sub- 
sequent discoveries  can  alone  impair  its  value.  Till 
^e  ardour  of  well-directed  enterprise  shall  disclose 
what  yet  remains  unexplored,  the  exposition  i>f  our 
actual  knowledge,  and  the  speculative  deductions  of 
enlightened  theory,  cannot  be  unacceptable  to  the 
lovers  of  geographical  research. 


•J  > 


March  1, 181«. 


UT'W 


THEfc 
near  api 
as  likewj 
and  Pac 
first  publ 
I  now 
they  con 
reaching 
be  fount 
geograp 
indeed, 
anewerc 
sage  (e^ 
in  seas 
packing 
Resolut 
voyage, 
Passage 


uidfl.  The 
uriouB,  «nd 
nployed  bj 
and  incle- 

as  complete 
North  Pole 
es,  and  with 
i  utmost  de- 
ipproached. 
d  the  Work 
mi,  indeed) 
eduction  of 
lents.  Sul>- 
value.  Till 
hall  disclose 
ution  of  oar 
eductions  of 
table  to  the 


h    •  i      ■'■'  J. 


V* 


PREFACE 


TO 


THE  FOLJLR  TRACTS. 


•  ■>■■     .. 


t     •  n' 


BTTHB 


HONOURABLE  DAIMES  BAREIMOTON. 


;« :.ii> 


'5f. 


ii  ^-t'   9  i-i"i  I  A,, 


XHE  following  Tracts,  relative  to  the  possibility  of 
near  approaches  to  the  Pole  of  our  own  hemisphere, 
as  likewise  of  a  communication  between  the  Atlantic 
and  Pacific  Oceans  in  any  Northern  direction,  were 
first  published  in  1775  and  1776* 

I  now  think  it  right  again  to  print  them,  because 
they  contain  many  well  attested  facts  with  regard  to 
reaching  high  NorUiem  Latitudes,  which  are  not  to 
be  found  elsewhere,  and  have  a  tendency  to  promote 
geographical  discoveries.  I  am  very  ready  to  admit, 
indeed,  that  the  purposes  of  commerce  can  never  be 
answered  by  the  great  uncertainty  of  a  constant  pas- 
sage (even  when  such  communication  is  discovered) 
in  seas  which  are  so  frequently  obstructed  by  the  ice 
packing  in  vast  fields.  I  find  likewise,  that  since  the 
Resolution  and  Endeavour  returned  from  their  last 
voyage,  many  conceive  a  North  East  or  North  West 
Passage  to  be  impracticable,  because  our  ships,  in 


k 


I 


\ 


i 


f.'Vi-Mrt*/;''' 


TUl 


PREFACE  TO  TH£ 


t 


vi 


'^  /«»V 


two  successive  years,  were  not  able  to  penetrate  be- 
yond 71%  by  impediments  of  ice.  Besides,  however, 
that  the  ice  packing  in  particular  situations  varies 
often  in  different  years,  both  these  attempts  were 
made  in  the  month  of  August,  which  I  flatter  myself  to 
have  proved,  is  the  very  season  of  the  year  when  the 
ice,  breaking  up  on  the  coast,  is  floating  in  every 
direction,  and  consequently  often  packs  in  masses 
of  an  immense  extent. 

These  vast  fields  of  ice,  indeed,  often  are  dispersed; 
but  who  hath,  or  indeed  should  have,  the  fortitude  of 
waiting  for  this  accident,  whilst  he  is  already  in  a  high 
Northern  Latitude,  and  the  winter  is  fast  approach- 
ing? If  the  ice,  however,  should  thus  pack  in  April 
or  May,  (which  I  conceive  it  would  not,  as  little  must 
be  left  to  float  from  the  preceding  summer,)  yet  as  the 
warm  weather  is  then  increasing  from  day  to  day,  the 
navigator  would  wait  with  some  degree  of  patience 
till  his  ship  may  be  released  from  this  temporary  ob- 
struction. The  situation  of  the  discoverer,  under 
these  circumstances,  may  be  compared  to  a  traveller 
passing  over  a  large  tract  of  sea  sand,  when  the  tide 
is  flowing  or  ebbing.  In  the  first  instance  he  spurs 
his  horse,  because  the  sea  may  be  expected  at  his 
heels ;  in  the  latter  he  proceeds  with  great  compo- 
sure, as  every  instant  he  loses  in  point  of  time  the  sea 
is  farther  removed.     "  •  >-         ' 

Others  again  have  despaired  of  a  Northwest  Pas- 
sage, from  Captain  Pickersgill  not  having  succeed- 
ed in  his  attempt  for  this  purpose  during  the  year 
1776.* 

'  *  In  the  Lion  armed  brig. 


r 


POLAR  TRACTS. 


#-■ 


IX 


lenetrate  be- 
es, however, 
itions  varies 
tempts  were 
tter  myself  to 
ear  when  the 
ing  in  every 
Ls  in  masses 

re  dispersed; 
e  fortitude  of 
>ady  in  a  high 
ist  approach- 
pack  in  April 
as  little  must 
;r,)  yet  as  the 
y  to  day,  the 
3  of  patience 
emporary  ob- 
(verer,  under 
to  a  traveller 
vhen  the  tide 
nee  he  spurs 
:pected  at  his 
great  compo- 
f  time  the  sea 

orthwest  Pas- 
ring  succeed- 
ring  the  year 


This  voyage  was  intended  for  two  purposes  (at 
least  as  I  have  been  informed ;)  the  first  to  protect 
some  of  our  whale  fishers  on  the  coast  of  West  Green- 
land from  the  Americans  then  in  rebellion ;  and  the 
second  (if  the  time  after  this  service  permitted)  to 
join  Captain  Cook,  should  he  have  been  so  fortunate 
as  to  have  accomplished  his  passage  fi:om  the  Pacific 
Ocean,  when  he  would  probably  have  returned  to 
England  by  Davis's  Straits. 

This  plan  seems  to  have  been  very  well  laid,  bui 
that  persevering  navigator  was  delayed  at  the  Cape 
by  Captain  Clark's  ship  not  arriving  till  a  considera- 
ble time  time  after  his  own  reaching  that  place  of  renr 
dezvous,  and  in  the  farther  progress  of  his  voyage  by 
adverse  winds,  which  drove  him  to  the  Friehdly  Isl- 
ands instead  of  Otaheite,  so  that  he  did  not  make  his 
attempt  of  a  passage  till  1777. 

Captain  Pickersgill  did  not  leave  Scilly  till  the  10th 
of  June,  1776,  and  consequently,  whatever  obstruc- 
tions he  met  with  from  floating  or  packing  ice,  might 
be  reasonably  expected  when  he  reached  the  coast  of 
West  Greenland.  It  appears,  however,  by  what  I 
shall  copy  from  the  conclusion  of  his  Journal  on  the 
31st  of  August,  that  he  did  not  find  these  to  be  consi- 
derable, and  that  after  the  trial  his  hopes  of  a  pas- 
sage were  very  sanguine. 

^'  I  shall  conclude  with  a  few  observation?  on  this 
part  of  the  world,  (sc.  Greenland)  and  so  terribly  re- 
presented by  people,  who,  in  order  to  raise  their  own 
merit,  make  dangers  and  difficulties  of  common  occur- 
rences, merely  because  the  places  arie  unknown,  and 
there  is  little  or  no  prol^ability  of  their  being  ever 

^    •  2- 


•*^ 


I 


t     ^^ 


*. 


m 


.*:* 


>#        * 


ll 


0  at''*  '  "^     '^f.  FREPACETOTHE 

• 

contradicted.    I  do  not  mean  this  as  a  personal  reflec- 
tion ;  but  having  discoursed  with  many  of  the  masters 
f:!  of  Greenland  vessels,  as  well  as  their  employers,  and 
'  heard  such  dreadful  stories  of  those  countries,  I  can- 

not help  remarking  it  as  tending  to  mislead  those  who, 
from  a  laudable  principle,  would  be  benefactors  to 
their  country,  but  are  deterred  from  it  by  these  mis- 
representations. I  shall  communicate  observations  on 
the  ice,  the  atmosphere,  the  land  of  Forbisher,  and 
the  probability  of  a  JVorthwest  Passage,  in  a  short  time*^* 

This,  however,  hath  unfortunately  been  prevented 
by  Captain  Pickersgill's  death;  but  the  Astronomer 
^    Royal,  who  communicated  Captain  PickersgilPs  Jour- 
nal to  the  Royal  Society,  hath  informed  me  by  letter, 
*«That  he   had  often  heard  this  navigator  express 
himself  as  well  assured  of  a  Northwest  Passage; 
adding,  that  he  received  accounts  of  it  from  the 
.  inhabitants  on  the  side  of  Davis^s  Straits,  and  that  it 
■'    was  directly  Northwest,  very  difierent  from  Baffin^s 
^      track. 

W  *  "'  ^^P^^!"  Pickersgill  likewise  thought,  that  the  best 
m  '  method  to  find  the  passage  was  to  get  out  early,  before  the 
ice  broke  away  in  the  upper  part  of  Davis* s  Straits." 
'  It  thus  appears,  that  the  last  attempts  of  a  North- 
west Passage  ended  with  the  officer's  employed 
thereon  being  thoroughly  persuaded,  that  it  was  not 
only  practicable,  but  highly  probable.  ^ 

As  the  late  geographical  discoveries  have  ^ven 
such  general  satisfaction,  I  have  little  doubt  but  that 
they  will  be  farther  prosecuted  when  a  peace  takes 


*  Phil.  Trans,  for  1 


74^pa||ii. 


p.  10i53. 


* 

'41 


.■r-.;^,. 


onal  reflec- 
|f  the  masten 
plojers,  and 
ntries,  I  can- 

those  who, 

nefactors  to 

by  these  mis- 

servations  on 

lorbisher,  and 

short  time.^* 

sen  prevented 

)  Astronomer 

ersgilPs  Jour- 

me  by  letter, 

rator  express 

est  Passage; 

r  it  from  the 

ts,  and  that  it 

from  Baffin^s 

lit,  that  the  best 
arlifi  before  the 
Straits:^ 
ts  of  aNorth- 
r's  employed 
bat  it  was  not 

!s  have  given 
oubt  but  that 
Bi  peace  takes 

Oft3.         ' -^w.'  . 


^10 


m 


POLAR  TKACT8. 


■0 


place,  and  shall  therefore  here  venture  to  throw  out 
my  poor  thoughts  with  regard  to  the  yet  remaining 
desiderata  for  the  more  perfect  knowledge  of  the 
planet  which  we  inhabit.  When  we  are  informed  by 
proper  trials,  that  the  attempt  in  any  particular  direc* 
tion  cannot  succeed,  we  shall  then  be  as  much  at  rest 
as  with  regard  to  Lunar  oceans  or  continents,  if  such 
there  be. 

I  have  mentioned  in  the  following  Tracts,  that  the 
Parliamentary  rewards  given  for  approaching  within 
one  degree  of  the  North  Pole  are  not  likely  to  pro- 
duce the  effects  intended,  because  the  Greenland 
whale  ships  are  all  ensured ;  if  they  were  therefore  to 
go  beyond  the  common  fishing  latitudes,  it  would  be 
such  a  departure  from  the  voyage  ensured,  that  they 
would  not  be  able  to  recover,  if  accidents  happened 
in  such  a  deviation,     j 

I  am  informed,  however,  that  there  are  some  vessels 
employed  in  time  of  peace  by  government,  to  prevent 
smuggling  on  the  Northern  Coast  of  Scotland.  These 
ships  might  be  instructed,  when  a  promising  wind 
blows  from  the  Southward,  to  proceed  as  far  North 
as  the  ice  will  permit.  The  crew  of  such  a  ship  would 
be  encouraged  by  expectations  of  the  Parl^ainentary 
reward ;  and  though  one  attempt  might  fail^  another 
might  succeed.  The  expense  to  the  public  v/ould  be 
trifling,  whilst  the  smugglers  would  not  know  how 
soon  the  ship  might  return  to  its  station. 

Our  Commodore  upon  the  Newfoundland  station 
might  also  send  a  vessel  at  a  small  expense,  to  explore 
all  the  Northern  part  of  Hudson's  Bay,  with  which  w« 
are  so  imperfectly  acquainted  at  present. 


*  > 


\: 


%". 


'?Wi 


4 


# 


# 


*      .*. 


,.^ 


J    V         V 


■• 


I.* 


'*% 


■i.-; 


Xll 


if*  .* 

fREFACE  TO  THE 


Such  attempts  during  peace  might  take  place  al- 
most every  summer;  and  I  should  suppose  that  this 
scientific  and  opulent  nation  would  never  hesitate 
%  *  (whilst  there  is  the  least  dawning  of  hopes)  to  send 
proper  vessels  occasionally  to  make  farther  trials 
both  of  a  Northwest  Passage  by  Baffin's  Bay,  and  a 
Northeast  beyond  Nova  Zembla.       '  ;>-.. ■!-«*, 

*  The  coasi.  of  Corea,  the  Northern  part  of  Japan, 

and  the  Lequieux  Islands,  should  also  be  explored ; 
the  cheapest,  and  perhaps  the  best,  method  of  doing 
this,  would  be  to  employ  a  vessel  in  the  India  Com- 
pany's service,  which  might  be  victualled  at  Canton. 
4  Thus  much  with  regard  to  discoveries,  or  better 

^owledge  of  the  more  unfrequented  parts  of  the 
"Northern  Hemisphere. 

The  desiderata  in  that  of  the  South  seem  to  be  the 
»  following: — 

To  make  the  complete  circumnavigation  of  New 
Holland,  so  as  at  least  to  be  better  acquainted  with 
some  parts  of  the  coast  of  this  immense  island ,  a  ves- 
sel for  this  purpose  might  be  victualled  at  the  Cape 
of  Good  Hope,  or  Canton :  nor  is  the  voyage  a  dis- 
tant one,  when  compared  with  those  of  Captain  Cook. 
New  Guinea  also  should  be  better  explored,  .•'^p..  >v 

We  scarcely  know  more  of  the  islands  of  Tristan 
da  Cunha  than  their  Longitude  and  Latitude;  but 
their  interior  parts  should  be  examined.  Not  vastly 
distant  is  Sandwich  Land,  which  many  on  board  Cap- 
tain Cook  supposed  to  be  a  vast  continent.  It  may 
be  objected,  indeed,  that  if  it  is  so,  it  will  turn  out  to 
be  a  continent  of  ice  and  snow ;  1  am  not  here,  how- 
ever, recommending  discoveries  for  the  purpose  of 


>*.  ■?:. 


L  ''j9r 

^■'^ 

1  JH 

■ 

^■ 

1 

"t.. 
'4-^ 

.♦.'■■ 


■-.^ 


^ 


f- 


"  -ii-?'^^5i^ii>***  -  .' 


^t^ 


POLAR  TRACTS.  Xui 

'     '     ■;  .■  -  .         ■"■;•  '     V 

commerce,    but   for    the    improvement  of  geogra- 
phy. 

I  should  conceive,  that  a  voyage  either  from  the 
Cape  or  Brazil  would  easily  give  opportunity  of  efiec- 
tuating  both  these  purposes. 

Perhaps,  whilst  discoveries  by  sea  are  thus  dwelt 
upon,  encouragement  should  be  given  to  travellers  by 
land,  forprocuring  better  information  with  regard  to  the 
central  parts  of  Asia,  Africa,  and  America.  In  short, 
let  us  endeavour  to  know  as  much  as  we  may  of  our 
globe ;  nor  should  this  be  considered  as  a  vain  and 
trifling  curiosity,  though  no  benefits  to  commerce  may 
result  from  these  inquiries. 


m  to  be  the 


*:       ■-■■ 


'  K', 


^. 


4i  ^■ 


f-i, 


r.  -.v'* 


^  .t^- 


m 


',,-.;•'.>■:,"•   ..  .•- 


■■*■  r-* ' ; . ,  - 


'•«..', 


f^X(  ^v>.  :_,.;.>,     /vj, 


^■■'^*' 


-Ay 


■%y 


■^'':J 


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f-'.-r,     I,. 


f    i^ 


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:*J 


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r 


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f: 


f 


t..V 


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'j':^«^7,F:^- 


:»: 


t 


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■*.  L* 


%     % 


"..*,»'■*'•  *'v*' 


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**J-t-<.     "^* 


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•<"*-•   « 


^if '  - 


/t  *^Jt"'^^ 


i' ,  ■  y 


"     % 


J0' 


^., — >_^, 


INSTANCES  OF  NAVIOATOBS 


WHO  BATt  KBACUD 


,^.. 

f 

^4 

^. 

.          r 

.4 

!T 

■'% 

' 

"4 

:*■: 

-    ,  .. 

' 

'ji 

HIGH  NORTHERN  LATITUDES. 


Read  at  a  Meeting  of  the  Royal  Society, 
MAY  19,  1774. 


-^♦' 


*<'^  if. 


■   \     -4 

As  I  was  the  unworthy  proposer  of  the  Voyage  to- 
wards the  North  Pole,  which  the  Council  of  the  Royal 
Society  recommended  to  the  Board  of  Admiralty,  I 
think  it  my  duty  to  lay  before  the  Society  such  intel- 
ligence as  I  have  happened  to  procure  with  regard  to 
navigators  having  reached  high  Northern  Latitudes  ;* 
because  some  of  these  accounts  seem  to  promise,  that 
we  may  proceed  farther  towards  the  Pole  than  the 
very  able  Officers,  whp  were  sent  on  this  destination 
last  year,  were  permitted  to  penetrate,  notwithstand- 
ing their  repeated  efibrts  to  pass  beyond  eighty  de- 
grees and  a  half. 

*  It  is  well  known  tbat  (here  are  many  such  accoaots  in  print, 
but  to  these  I  need  not  refer  the  Society. 


P' 


V 


-     » ■    > 


■  I     * 


.4 


'■% 


0 


f 
4 


It'  f 


\'l 


16 


M-m 


m.   ' ' 

ON  APPROACHINCJ 


I  shall  begin,  however,  by  making  an  observation 
;   or  two  with  regard  to  the  Greenland  Fishery,  which 
will  in  a  great  measure  account  for  our  not  being  able 
to  procure  many  instances  of  nearer  approaches  to 
^.       the  Pole  than  the  Northern  parts  of  Spitzbergen. 
'"■  Fifty  years  ago,  such  apprehensions  were  enter- 

tained of  navigating  even  in  the  loose,  or  what  is 
called  sailing  ice^  that  the  crews  commonly  continued 
.    on  shore,*  from  whence  they  only  pursued  the  whales 
'     in  boats. 

The  demand,  however,  for  oil  increasing,  whilst 
the  number  offish  rather  decreased,  they  were  obliged 
1**  * '  to  proceed  to  sea  in  quest  of  them^  and  now,  by  expe- 

rience and  adroitness,  seldom  suffer  from  the  obstruc- 
tions of  ice/|* 

The  masters  of  ships,  who  are  employed  in  this 
trade,  have  no  other  object  but  catching  whales, 
which,  as  long  as  they  can  procure  in  more  Southern 
Latitudes,  they  certainly  will  not  go  in  search  of  at 
a  greater  distance  from  the  port  to  which  they  are  to 
;^  return :  they,  therefore,  seldom  proceed  much  beyond 
eighty  degrees  North  Latitude,  unless  driven  by  a 
strong  Southerly  wind  or  other  accident. 

Whenever  this  happens,  also,  it  is  only  by  very 
•     diligent  inquiries  that  any  information  can  be  procur- 
ed ;  for  the  masters,  not  being  commonly  men  of  sci- 

'     *  There  were  houses  still  standing  on  Spitzbergen,  where  the 
Dutch  used  to  boil  their  train  oil. — Marten's  Voyage,  p.  24.     See 
•«  \      also  Callander,  vol.  iii.  p.  723.  -,;   t'^ 

t  These  particulars  I  received  from  Captain  Robinson,  whom  I 
shall  have  hereafter  occasion  to  mention.  > '. 


■y-%^. 


t'H 


% 


>t 


,&': 


"i"**ii*«^. 


* 


observation 
tiery,  which 
it  being  able 
proaches  to 
sbergen. 
were  enter- 
,  or  what  is 
ily  continued 
d  ^he  whales 

asing,  whilst 
were  obliged 
low,  by  expe- 
1  the  obstruc- 

ioyed  in  this 
hing  whales, 
ore  Southern 
search  of  at 
:h  they  are  to 
much  beyond 
driven  by  a 
t. 

only  by  very 
an  be  procur- 
ly  men  of  sci- 

irgen,  where  the 
age,  p.  24.     See 

.obiDSon,  whom  I 

>     .  ■    '■  t--    -1^  •  •  ■;* 


THE  NORTH  POLE. 

ence,  or  troubling  their  heads  about  the  improvement 
of  geographical  knowledge,  never  mention  these  cir- 
cumstances on  their  return,  because  they  conceive 
that  no  one  is  more  interested  about  these  matters 
than  they  are  themselves.  Many  of  the  Greenland 
masters  are  likewise  directed  to  return  after  the  early 
fishery  is  over,  provided  they  have  tolerable  success ; 
so  that  they  have  no  opportunity  of  making  disco- 
veries to  the  Northward. 

To  these  reasons  it  may  be  added,  that  no  ships 
were  perhaps  ever  sent  before  last  summer  with  ex- 
press instructions  to  reach  the  Pole,  if  possible,  as 
most  other  attempts  have  been  to  discover  a  North- 
east or  Northwest  Passage,  which  were  soon  defeat- 
ed by  falling  in  with  land,  or  other  accident. 

Having  thus  endeavoured  to  show  that  the  instan- 
ces of  ships  reaching  high  Northern  latitudes  must 
necessarily  be  rare,  1  shall  now  proceed  to  lay  before 
the  Society  such  as  I  have  been  able  to  hear  of  since 
the  voyage  towards  the  North  Pole  was  undertaken 
during  last  summer. 

When  this  was  determined  upon,  and  mentioned  in 
the  newspapers,  it  became  matter  of  conversation 
amongst  the  crews  of  the  guard-ships ;  and  Andrew 
Leekie,  an  intelligent  seaman  on  board  the  Albion 
(then  stationed  at  Plymouth,)  informed  some  of  the 
officers  that  he  had  been  &s  far  North  as  84?". 

When  he  was  asked  farther  on  this  head,  he  said 
that  he  was  on  board  the  Reading,  Captain  Thomas 
Robinson,  in  1766,  and  that,  whilst  he  was  shaving 
the  Captain,  Mr.  Robinson  told  him,  that  he  had 
probably  never  been  so  far  to  the  Northward  before. 

3 


# 


I 


tn 


4>r 


^t 


!■'    5v 


M-^n 


% 


^Uk^' 


«.' 


'4 


w 


UN  APPROACHING 


■«r- 


as  they  had  now  reached  the  above-mentioned  degree 
of  latitude. 

Having  happened  to  hear  this  account  of  Lcekie*s, 
on  ray  return  to  London  this  winter,  I  found  out  Cap- 
tain Robinson,  who  remembered  his  having  had  this 
conversation  with  Leekie ;  but  said,  that  ho  was  mis- 
taken in  supposing  that  they  had  reached  04^"  North 
latitude,  as  they  were  only  in  82i*. 

Captain  Robinson  then  explained  himself,  that  he 
had  at  this  time  computed  his  latitude  by  the  run 
back  to  Hakluyt's  Headland  in  twenty-four  hours  j 
from  which,  and  other  circumstances  mentioned  in 
iny  presence  before  two  sea-officers,  they  told  me 
afterward,  that  they  had  little  or  no  doubt  of  the 
accuracy  of  his  reckoning.  Mr.  Robinson  likewise 
remembers  that  the  sea  was  then  open,  so  that  he  hath 
no  doubt  of  being  able  to  reach  83%  but  how  much 
farther  he  will  not  pretend  to  say,  t 

This  same  Captain,  in  the  ship  St.  George,  was,  on 
the  |5th  of  June,  1773,  ip  North  latitude  81'  16',  by 
a  very  accurate  observation  with  an  approved  Had-< 
ley*s  quadrant,  in  which  he  also  made  the  proper 
allowance  for  the  refraction  in  high  Northern  lati-* 
tudes ;  at  which  time  seeing  some  whales  spouting  to 
the  Northward,  he  pursued  them  for  five  hours,  so 
that  he  must  have  reached  811,  when  the  sea  was 
open  to  the  Westward  and  East  Northeast  as  far 
as  he  could  distinguish  from  the  mast-head.  His 
longitude  was  then  3"  East  firom  the  meridian  of 
iLondon. 

Captain  Robinson  is  a  very  intelligent  seaman,  and 
hath  navigated  the  Greenland  Sea§  these  twentyyeayg, 


*  He 
Dock, 
Greenlan 
tilde  81* 
that  evid 

t  See] 
A.  D.  1( 
sumtnerJ 

They] 
Februar 
light  of  I 
Ibid. 


'  M 


■>;*ttsi»^l 


'tHS,  NORTH  Pott, 


10 


If,  that  he 
by  the  run 
four  hours; 
entioned  in 
ey  told  me  « 
»ubt  of  the 
on  likewise 
that  he  hath 
t  how  much 

)rge,  was,  on 
3  81M6',  by 
proved  Had-' 
5  the  proper 
orthern  lati- 
:s  spouting  to 
ive  hours,  so 

the  sea  was 
theast  as  far 
»t-head.    His 

meridian  of 

•V^   W  '  ■ 
seaman,  and 

I  twentyyearg^ 


.1 


except  during  the  interval  that  he  was  employed  by 
the  Hudson^s  Bay  Company* 

I  could  add  some  other,  perhaps  interesting,  parti'> 
culars,  which  I  have  I'eceived  from  Captain  Robin* 
son,  with  regard  to  Spitzbergen  and  the  Polar  Seas ; 
I  will  only  mention,  however,  that  he  thinks  he  could 
spend  a  winter  not  uncomfortably  in  the  most  North- 
em  parts  we  are  acquainted  with,t  as  there  are  threci 
or  four  small  settlements  of  Russians  in  this  country, 
for  the  sake  of  the  skins  of  quadrupeds,  which  are 
then  more  valuable  than  if  the  animal  is  taken  in 
summer.     "  !.    ■:*  ^ 

■'■  The  next  instance  I  shall  mention  of  a  navigator, 
who  hath  proceeded  far  Northward,  is  that  of  Captain 
Cheyne,  who  gave  answers  to  certain  queries  dranhi 
up  by  Mr.  Dalrymple,  F.R.S.  in  relation  to  the  Polar 
Seas,  and  which  were  communicated  kst  year  to  the 
Society. 

Captain  Cheyne  states,  in  this  paper,  diathehath 
been  as  far  as  North  latitude  82** ;  but  does  not  spe- 
cify whether  by  observation  or  his  reckoning,  though 

*  He  lived  during  this  winter  in  Queen-street,  near  Greenland 
Dock,  Rotherhithe  ;  he  hath  sailed,  probably,  by  this  time  on  the 
Greenland  Fishery.  With  regard  to  his  having  been  in>North  lati- 
tude 81°  30',  in  June,  1773,  he  can  prove  it  by  his  Journal,  if 
that  evidence  should  be  required. 

t  See  the  Narrative  of  eight  sailors,  who  wintered  in  Greenland 
A.  D.  1630,  and  who  all  returned  in  health  to  England  the  ensuing 
summer. — Churchill's  Voyage,  vol.  iv.  p.  811. 

They  did  not  see  the  sun  from  the  14th  of  October  till  the  Sd  of 
February.  By  the  last  day  of  January,  however,  they  had  day- 
light of  eight  hours.    They  wintered  in  North  latitude  77 — 4o.'~- 


•>*•' 


\- 


..-»,.*-*iita*'£^: 


M:,.^r 


ijijfS--^'s..- 


20 


•N  ArPnOACHlNO 


irom  many  other  anawers  to  the  iiiterrogatoriei  pro- 
posed, it  should  seem  that  he  speaks  of  the  latitude 
by  observation.  Unfortunately  Captain  Cheyne  ia  at 
present  on  the  coast  of  Africa,  so  that  farther  infor- 
mation on  this  head  cannot  be  now  procured  from 
him. 

Whilst  the  ships  destined  for  the  North  Pole  were 
preparing,  a  most  ingenious  and  able  Sea-Officer, 
Lieutenant  John  Cartwright,  told  me,  that  twelve 
years  ago  he  had  been  informed  of  a  very  remark- 
able voyage  made  by  Captain  Mac-Callam  as  far 
nearly  as  84°  North  latitude. 

This  account  Mr.  Cartwright  had  received  from  a 
brother  Officer,  Mr.  James  Watt,  now  a  Master  and 
Commander  in  the  Royal  Navy,  who  waa  on  board 
Captain Mac-Callam's  ship. .  t     ..^^, , 

I  thought  it  my  duty  to  acquaint  the  Admiralty  with 
this  intelligence,  who  would  have  sent  for  Mr.  Watt, 
lt>ut  he  yyaa  then  employed  on  the  coast  of  America. 

On  his  return  from  thence,  within  the  last  month, 
Mr.  Cartwright  introduced  a  conversation  with  regard 
to  Captain  Mac-Callam's  voyage,  when  Mr.  Watt  re- 
peated all  the  circumstances  which  he  had  mentioned 
to  him  twelve  years  ago ;  after  which  Mr.  Cartwright, 
thinking  that  I  should  be  glad  to  hear  the  particulars 
from  Mr.  Watt  himself,  was  so  good  as  to  bring  him 
to  my  chambers,  when  I  received  from  him  the  fol- 
lowing information. 

In  the  year  1751  Mr.  Watt,  then  not  quite  seventeen 
years  of  age,  went  on  board  the  Campbeltown  of 
Campbeltown,  Captain  Mac-Callam,  which  ship  was 
at  that  time  employed  in  the  Greenland  Fishery. 


I 


It  seei 
suppose 
vessels  ^ 
Capta 
able  an<] 
the  Norl 
the  8eas( 
trating  fs 
fore  the  1 
ceeded  v 
sea  was 
had  not  i 
and  the  i 
short.  Ml 
sant  navij 
It  need 
83i'was( 
jectofthi 
^  therefore 
I  cd  the  la( 
Hadley's 
^  departure 
"^Headlanc 
When 
3  em  latitu 
■I  was  not  s 
ed  from 
ing  that 
blamed  b 
tainly  by 
^against  tf] 


At 


•— tJr;:.:;-.^***^- 


TKS  irORTH  POLE. 


ones  pro- 
\e  latitude 
eyne  ia  at 
•ther  infor- 
:ured  from 

Pole  were 
)ea-Officer, 
hat  twelve 
fry  remark- 
ilam  as  far 

Ived  from  a 
Master  and 
dA  on  board 

miralty  with 
^r  Mr.  Watt, 
America, 
last  month, 
with  regard 
At.  Watt  re- 
d  mentioned 
Cartwright, 
;  particulars 
to  bring  him 
him  the  fol- 

te  seventeen 
pbeltown  of 
ich  ship  was 
i'ishery. 


It  seems,  that,  during  the  time  the  whales  are 
supposed  to  copulate,  the  crews  of  the  Greenland 
vessels  commonly  amuse  themselves  on  shore. 

Captain  Mac-Callam,  however,  (who  was  a  very 
able  and  scientific  seaman,)  thought  that  a  voyage  to 
the  North  Pole  would  be  more  interesting ;  and  that, 
the  season  being  a  fine  one,  he  had  a  chance  of  pene- 
%  trating  far  to  the  Northward,  as  well  as  returning  be- 
fore the  later  fishery  took  place.  He  accordingly  pro- 
ceeded without  the  least  obstruction  to  83i%  when  the 
sea  was  not  only  open  to  the  Northward,  but  they 
had  not  seen  a  speck  of  ice  for  the  last  three  degrees, 
and  the  weather  at  the  same  *ime  was  temperate ;  in 
short,  Mr.  Watt  hath  never  experienced  a  more  plea- 
sant navigation. 

It  need  be  scarcely  observed,  that  the  latitude  of 
83^**  was  determined  by  observation,  as  the  great  ob- 
ject of  the  voyage  was  to  reach  the  Pole ;  the  Captain, 
therefore,  the  Mate,  and  young  Mr.  Watt,  determin- 
ed the  latitude  from  time  to  time,  both  by  Da;vis  and 
'Hadley's  quadrants:  to  this  I  may  add,  that  their 
)  departure  and  return  were  from  and  to  Hakluyt'g 
'  Headland. 

When  they  were  advancing  into  these  high  North- 
f  em  latitudes,  the  Mate  complained  that  the  compass 
I  was  not  steady,  on  which  Captain  Mac-Callam  desist- 
;|cd  from  his  attempt,  though  with  reluctance;  know- 
ling  that  if  any  accident  happened,  he  should  be 
'blamed  by  his  owners,  who  would  be  reminded  cer- 
tainly by  the  Mate  of  the  protests  he  had  made 
:|against  the  ship's  proceeding  farther  Northward,  v 


\ 


*. 


\ 


** 


'i&l,.- 


:^" 


*^'- 


22 


ON  APPROACHING 


i- 


Several  of  the  crew,  however,  were  for  prosecuting 
their  discoveries,  and  Mr.  Watt  particularly  remem- 
bers the  chagrin  which  was  expressed  by  a  very 
intelligent  seaman,  whose  name  was  John  Kelly; 
Captain  Mac-Callam,  also,  after  his  return  from  that 
voyage,  hath  frequently  said,  in  the  presence  of  Mr. 
Watt  and  others,  that,  if  the  Mate  had  not  been  faint- 
hearted, the  ship  possibly  might  have  reached  the 
Pole. 

Both  Captain  Mac-Callam  and  the  Mate  are  now 
dead,  and  it  is  rather  doubtful  whether  the  ship^s 
Journal  can  be  procured.  -'f***^  ^^^  ^*^' 

It  remains  therefore  to  be  considered  what  may  be 
objected  to  the  credibility  of  this  very  interesting 

account.  .     _..  ,  .i^T'>i»T>;i^.??u-rv  . 

I  have  stated,  that  Mr.  Watt  was  not,  at  the  time 
this  voyage  took  place,  quite  seventeen  years  of  age : 
but  I  have  also  stated,  that  he  observed  himself  (as 
well  as  the  Master  and  Mate)  from  time  to  time.  Is 
it  therefore  more  extraordinary  he  should  remember 
with  accuracy,  that,  two  and  twenty  years  ago,  he 
had  been  in  North  latitude  831%  than  that,  at  the  same 
distance  of  time,  he  might  recollect  that  he  had  been 
at  a  friend's  house,  which  was  situate  eighty-threr 
miles  and  a  half  from  London  ?  Or  rather,  indeed,  is 
not  his  memory,  with  regard  to  this  high  latitude, 
much  more  to  bt  depended  upon,  as  the  circumstance 
is  so  much  more  interesting,  especially  as  Mr.  Watt 
was  even  then  of  a  scientific  turn  ? 

To  this  I  may  add,  that  it  being  his  first  voyage, 
and  so  remarkable  an  one,  Mr.  Watt  now  declares 


upon. 

IfM 
this  obj 
lam's  fr 
of  the 
have  re 
conceiF 
have  be 
But   i 
took  pla 
fore,  at 
can  be  r 
It  is  ti 
tempt  ir 
the  folio 
traversii 
^  the  rec< 
precedii 
farther 
This, 
already 


-««. 


■■■"•^'t-. 


%. 


■0- 


THIS  NORTH  POLE. 


23 


prosecuting 
arly  remem- 
by  a  very 
ohn  Kelly; 
irn  from  that 
sence  of  Mr. 
ot  been  faint- 
reached  the 

late  iire  now 
er  the  ship's 

what  may  be 
ry  interesting 

>t,  at  the  time 
years  of  age; 
ed  himself  (as 
ne  to  time.    Is 
mid  remember 
years  a^o,  he 
hat,  at  the  same 
lat  he  had  been 
te  eighty-three 
ither,  indeed,  is 
9  high  latitude, 
le  circumstance 
lly  as  Mr.  Watt 

his  first  voyage, 
,tt  now  declares 


<•'? 


that  he  remembers  more  particulars  relative  to  it, 
than  perhaps  in  any  other  since  that  time :  other  sea- 
officers  have  likewise  told  me,  that  the  circumstances 
of  their  first  voyages  are  most  fresh  in  their  memory, 
the  reason  for  which  is  too  obvious  to  be  dwelt 
upon. 

If  Mr.  Watt's  recollection  however  is  distrusted, 
this  objection  extends  equally  to  Captain  Mac-Cal- 
lam's  frequent  declarations,  that,  if  the  apprehensions 
of  the  Mate  had  not  prevented,  he  might  possibly 
have  reached  the  North  Pole :  and  how  could  he  have 
conceived  this,  unless  he  had  imagined  himself  to 
have  been  in  a  very  high  Northern  latitude  ?    :         -^ 

But  it  may  be  possibly  said,  that  this  voyage 
took  place  above  twenty  years  since,  and  that  there- 
fore, at  such  a  distance  of  time,  no  one's  memory 
can  be  relied  upon. 

It  is  true  indeed,  that  Mac-Callam  made  this  at- 
tempt in  1751 ;  but  Mr.  Watt  continued  his  services 
the  following  year  in  a  Greenland  ship,  and  therefore, 
traversing  nearly  the  same  seas,  must  have  renewed 
the  recollection  of  what  he  had  experienced  in  the 
preceding  voyage,  though  he  did  not  then  proceed 
farther  than  North  latitude  80^ 

This,  however,  brings  it  only  to  1752;  but  I  have 
already  stated,  that  within  these  twelve  years  he 
mentioned  all  the  particulars  above  related  to  his 
brother-ofiicer.  Lieutenant  Cartwright. 

Mr.  Watt  also  frequently  conversed  with  Captain 
Mac-Callam  about  this  voyage  after  both  of  them  had 
quitted  the  Greenland  ships ;  Mr.  Watt  rising  regu- 
larly to  be  a  Master  and  Commander  in  His  Majesty's 


4 


-f 


1- 


% 


^fr 


m 


ON  AI^KOACHING 


i  '■ 


<  ■ 


service^  and  Captain  Mac-Callam  becoming  Purser 
of  the  Tweed  Man  of  War. 

It  so  happened,  that  in  the  year  of  the  expedition 
against  Bellisle,  Mr.  Watt,  Captain  Mac-Callam,  and 
Mr.  Walker  (comitaonljr  called  Commodore  Walker, 
from  his  having  commanded  the  koyal  Family  pri- 
Tateers  in  the  late  war,)  met  together  at  Portsmouth, 
when  they  talked  over  the  circumstances  of  this 
^^ ;.  Greenland  voyage,  which  Mr.  Walker  was  interested 
in,  by  having  been  the  principal  owner  of  the  Camp- 
beltown. 

Mr.  Watt  and  Captain  Mac-Callam  met  also  eleven 
years  ago  in  London,  when  they  as  usual  conversed 
about  the  having  reached  so  high  a  Northern  lati- 
tude. 

1  now  come  to  my  last  proof,  which  I  received  from 
the  late  Dr.  Campbell,  the  able  continuator  and  revi- 
ser of  Harris's  Collection  of  Voyages. 

In  that  very  valuable  compilation,  Commodore 
Roggewein's  circumnavigation  makes  a  most  material 
addition,  some  of  the  most  interesting  particulars  of 
which  were  communicated  by  Dr.  Dallie,  who  was  a 
native  of  Holland,*  and  lived  in  Racquet  Court,  Fleet 
Street,  about  the  year  1745,  where  he  practised 
physic. 

Dr.  Campbell  went  to  thank  Dallie  for  the  having 
furnished  him  with  Roggewein's  Voyage,  when  Dallie 
said,  that  he  had  been  farther  both  to  the  Southward 
and  to  the  Northward  than  perhaps  any  other  person 
who  ever  existed.  --^  ''  r  ^      :  ^  ^^ 

I* 

*  He  was  a  grandson  of  Dallie,  who  was  author  of  a  book,  much 


•stecmcd  by  the  Divines,  entitled  "/5c  Urn  Pat 


rum. 


X 


\:^-^\^i}"' 


Puwer 

pedition 
am,  and 
Walker, 
nily  pri- 
tsmouth, 
of  this 
terested 
eCamp- 

o  eleven 
mversed 
em  lati- 

red  from 
^d  revi- 

imodore 
material 
lulars  of 
10  was  a 
pt,  Fleet 
ractised 

having 
n  Dallie 
ithward 

person 

ok,  much 


^■~  ^M 


.  1^ 


W 


TB  MOKm  POLE. 


2S 


~  fie  then  explained  himself  as  to  the  haying  Iksen 
in  high  Southern  latitudes,  bj  sailing  in  Roggewein^s 
fleet;*  and  as  to  his  having  been  &r  to  the  North- 
ward, he  gave  the  following  account:— 

Between  fif^  and  sixty  years  ago  it  was  usual  to 
send  a  Dutch  ship  of  war  to  superintend  the  Green- 
land fishery,  though  it  is  not  known  whether  this 
continues  to  be  a  regulation  at  present 

Dr.  Dallie  (then  young)  was  on  board  the  Dutch 
vessel  employed  on  this  service  ;t  and,  during  the 
interval  between  the  two  fisheries,  the  Captain  deter- 
mined, like  Mr.  Mac-Callam,  to  try  whether  he  could 
not  reach  the  Pole;  and  accordingly  penetrated  (to  the 
best  of  Dr.  Campbell's  recollection)  as  far  as  North 
latitude  88°,  when  the  weather  was  warm,  the  sea 
perfectly  free  from  ice,  and  rolling  like  the  Bay  of 
Biscay.  DaUie  now  pressed  the  Captain  to  proceed ; 
but  he  answered,  that  he  had  already  gone  too  far 
by  having  neglected  his  station,  for  which  he  should 
be  blamed  in  Holland :  on  which  account,  also,  he 
would  suffer  no  Journal  to  be  made,  but  returned  a9 
speedily  as  he  could  to  Spitzbergen. 

There  are  undoubtedly  two  objections,  which  may 
be  made  to  this  account  of  Dr.  Dallie's,  which  are, 
that  it  depends  not  only  upon  his  own  memory,  but 
that  of  Dr.  Campbell,  as  no  Journal  can  be  produced, 
for  the  reason  which  I  have  before  stated. 

*  Roggewein  reached  South  latitude  62°  3(f. — See  Harris. 

1  Dr.  Campbell  does  not  recollect  in  what  capacity  he  served : 
but,  as  he  afterward  practised  physic,  he  might  probably  hav« 
been  the;  surfeon. 


'*' « 


'     ,?^> 


^• 


"i^i 


l» 


¥ 


% 


_^,_    HIII.IIIIHI  I  I      -, 


■•■' ji«»fiMr-T'*»"wk*t.ttjttt;.  - 


26 


m 


V  -  ffV.  ■ 

i 

ON  APrROACHINO 


[^l: 


The  conversation,  however,  between  Dr.  Campbell 
and  Dallie,  arose  from  the  accidental  mention  of 
Roggewein^s  voyage  to  the  Southward;  and  can  it 
be  supposed  that  Dallie  invented  this  circumstantial 
narrative  on  the  spot,  without  having  actually  been  in 
f>     a  high  Northern  latitude  ? 

If  this  be  admitted  to  have  been  improbable,  was 
he  not  likely  to  have  remembered  with  accuracy 
what  he  was  so  much  interested  about,  as  to  have 
pressed  the  Dutch  Captain  to  have  proceeded  to  the 
Pole? 

*  But  it  may  be  said,  also,  that  we  have  not  this 
account  from  Dallie  himself,  but  at  second-hand  from 
Dr.  Campbell,  at  the  distance  of  thirty  years  from 
the  conversation. 

1  To  this  it  may  be  answered,  that  Dr.  Campbell's 
memory  was  most  remarkably  tenacious,  as  is  well 
known  to  all  those  who  had  the  pleasure  of  his 
acquaintance ;  and,  as  he  hath  written  so  ably  for  the 
promotion  of  geographical  discoveries  in  all  parts  oi 
the  globe,  such  an  account  could  not  but  make  a 
strong  impression  upon  him,  especially  as  he  received 
it  just  after  the  first  edition  of  his  compilation  of 
voyages. 

No  one  easily  forgets  what  is  highly  interesting  to 
him ;  and,  though  I  do  not  pretend  to  have  so  good  a 
memory  as  Dr.  Campbell,  I  have  scarcely  a  doubt, 
but  that,  if  I  should  live  thirty  years  longer,  and 
retain  my  faculties,  I  shall  recollect  with  precision 
^  every  latitude  which  I  have  already  stated  in  this 
Paper.  "' 


%^ 


■'■%i**,r'    ;'_ 


^ 


*'>fm*m-jmm 


ampbell 
ntion  of 
can  it 
istantial 
been  in 

>le,  was 

ccuracy 

to  have 

d  to  the 

not  this 
Lndfrom 
JTs  from 

npbell*s 
is  well 
of  his 
'  for  the 
parts  of 
make  a 
eceived 
ition  of 

»ting  to 
good  a 
doubt, 
ir,  and 
ecision  .* 
in  this 


It 


1^ 

THE  NORTH  POLE. 


*■• 


What  credit,  however,  is  to  be  given  to  all  thisse 
narratives  is  entirely  submitted  to  the  Society,  as  I 
have  stated  them  most  fully,  with  every  circumstance 
which  may  invalidate,  as  well  as  support  them ;  and, 
if  I  have  endeavoured  to  corroborate  them  by  the 
observations  which  I  have  made,  it  is  only  because  ! 
believe  them. 

It  should  seem  upon  the  whole  of  the  inquiries  on 
this  point,  that  it  is  very  uncertain  when  ships  may 
proceed  far  to  the  Northward  of  Spitzbergen ;  and 
that  it  depends,  not  only  upon  the  season,  but  other 
accidents,  when  the  Polar  Seas  may  be  so  free  from 
ice  as  to  permit  attempts  to  make  discoveries.* 

Possibly,  therefore,  if  a  King's  officer  was  sent 
from  year  to  year  on  board  one  of  the  Greenland 
ships,  the  lucky  opportunity  might  be  seized,  and  the 
Navy  Board  might  pay  for  the  use  of  the  vessel,  if  it 
was  taken  from  the  whale  fishery,  in  order  to  pro- 
ceed as  far  as  may  be  towards  the  North  Pole. 

*  Captain  Robinson  hath  infonned  me,  that  at  the  latter  end  of 
last  April  a  Whitby  Ship  was  in  North  latitude  80**,  without  having 
been  materially  obstructed  by  the  ice.  Captain  Marshall  was  also 
oS  Hakluyt's  Headland  so  early  as  the  25th  April,  without  ohserr- 
ing  much  ice. 


Kr 


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ADDITIONAL  PROOFS,  ISjc. 


■>;-,''<-'^'i«i7 

■'■^•■•■■.■.■*wti 

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?(?:•  -^^  ^^iii 

■livv'-"^^' 

'    '•  4 

^v-% 

■  :^^ 

Read  at  a  Meetii^  of  Ae  Royd  Society. 
DEC.  Sf.  1774. 


AjB  I  happened  to  have  collected  many  additional 
facts  since  my  paper,  containing  Instances  of  Naviga- 
tors who  had  reached  high  Northern  latitudes,  was 
read  hefore  the  Society  in  May  last,  I  shall  take  the 
liberty  to  state  them  according  to  chronolo^cal 
order;  t<^ether  with  some  general  reasons  why  it 
may  be  presumed,  that  the  Polar  Seas  are,  at  least 
sometimes,  navigable. 

I  think  it  my  duty  to  do  this,  not  only  because  I 
was  the  unworthy  proposer  of  the  Pdlar  voyage  in 
1773,  which  was  recommended  by  the  Council  of  the 
Royal  Society  to  the  Board  of  Admiralty ;  but  be- 
cause it  would  not  redound  much  to  the  credit  of  the 
Sofiiiity,  if  they  planned  a  voyage  to  reach  the  North 
Pole,  if  possible,  when  a  perpetual  barrier  of  ice 
prevented  any  discoveries  in  the  Spitzbei^en  seas  to 
the  Northward  jf  80^%  which  is  not  a  degree  beyond 
the  most  common  station  of  the  Greenland  fishers,  -^"■ 

I  must  here,  however,  repeat,  that  no  one  is  more 
entirely  satisfied  than  myself  of  the  great  abilities, 
perseverance,  and  intrepidity,  with  which  the  offi- 


■^-. 


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cers,  who  were  sent  on  this  destinatioHf  attempted  to 
prosecute  their  discoveries ;  but  I  conceive,  from  the 
arguments  and  facts  which  will  follow,  that  thej 
were  stopped  by  a  most  unfortunate  barrier  of  ice 
(of  great  extent  indeed)  but  which  was  only  tem- 
porary and  not  perpetual. 

If  such  a  wall  of  ice  hath  been  constantly  fixed  in 
this  latitude,  and  must  continue  to  be  so,  there  is  an 
end  to  all  discoveries  to  be  made  to  the  northward 
of  Spitzbergen;  but  if  it  is  only  occasional,  the 
attempt  may  be  resumed  in  some  fortunate  year.'^ 

The  point  therefore  being  of  so  much  importance 
to  geography^  I  hope  the  Society  will  pardon  me,  if  I 
more  fully  enter  into  the  subject  than  I  did  in  my 
former  Paper, 

The  English  have  long  taken  the  lead  in  geogra- 
phical discoveries.  One  of  our  ships  of  war  is  lately 
returned,  after  having  penetrated  into  the  Antarctic 
Circle ;  and  is  it  not  rather  a  reflection  upon  a  scien- 
tific nation,  that  more  is  not  known  with  regard  to 
the  circumpolar  regions  of  our  own  hemisphere,  than 
can  be  collected  from  maps  made  in  the  time  of 
Charles  I.  especially  when  the  run  from  tte  mouth  of 
the  Thames  to  the  North  Pole  is  not  a  longer  one 
than  from  Falmouth  to  the  Cape  de  Yerd  Islands  .^ 

Thoi^h  I  have  the  honour  to  be  a  Fellow  of  a 
Society  instituted    for   the    promotion    of  Natural 

*  Upon  the  first  return  of  the  king's  ships  from  the  Polar  Voyage, 
this  notion  of  a  perpetual  barrier  of  ice  at  North  latitude  801"  ^^^^ 
prevailed  so  much,  that  some  very  distinguished  philosophers  of 
fliis  country  had  shown  thoughts  of  proceeding  to  the  Pole  over  the 
ice,  in  such  a  wind  boat  as  the  Dutch  have  sometimes  made  use  of. 


Ai" 


Jf' 


.4" 


■'^■v 


t. 


•H  -ti       "If 


ipted  to 
rom  the 
at  thej 
of  ice 
\y  tem- 

Sxed  in 
re  is  an 
thward 
al,  the 
far.* 
ortance 
me,  if  I 
in  my 


^•r 


geogpa- 
s  lately 
ntaretic 
I  scien- 
;ard  to 
'e,  than 
time  of 
outh  of 
er  one 
ids? 
w  of  a , 
Fatural 

Voyage, 
Ol'had 
•hers  of 
•ver  the 
use  of. 


J!^'' 


*-,'■ 

■'■& 


THE  NORTH  POLE. 


tfl 


Knowledge,  the  prejudices  of  an  Englishmem  are  so 
strong  with  me,  that  I  cannot  but  wish  the  discoveries 
to  be  made  in  the  Polar  Seas  may  be  achieved  by 
my  countrymen ;  but,  if  we  are  determined  to  aban- 
don the  enterpris :,  science  is  to  be  honoured  from 
whatever  quarter  it  may  come,  and  it  hath  therefore 
given  me  gr«at  satisfaction  to  hear,  that  Mons.  de 
Bougainville  is  soon  to  be  sent  on  discoveries  to  the 
Northward.* 

In  the  outset  of  my  former  Paper,  I  said  I  should 
not  trouble  the  Society  with  any  instances  of  naviga- 
tors having  reached  high  Northern  Latitudes,  which 
had  appeared  in  print.  During  the  course  of  this 
summer,  however,  I  have  happened  to  find  three 
such  accounts,  which  were  never  before  alluded  to, 
and  which  are  extracted  from  books  that  are  not 
commonly  looked  into,  or  at  least  often  consulted 
upon  points  of  geography. 

When  the  Royal  Society  was  first  instituted,  it  was 
usual  to  send  queries  to  any  traveller  who  happened 
to  reside  in  England,  after  having  been  in  parts  of 
the  world  which  are  not  commonly  frequented.t 

In  the  year  1662-3,  Mr.  Oldenburgh,  the  Secretary 
of  the  Society,  was  ordered  to  register  a  Paper, 
entitled,  "  Several  Inquiries  concerning  Greenland, 
answered  by  Mr.  Grey,  who  had  visited  those  parts." 

*  I  have  since  been  informed,  that  this  intended  voyage  wai 
dropped,  by  the  French  Minister  for  the  marine  department  being 
changed.      .-i"  "■•,   '-■■'''• ''iifi-n^rvii  '■■'v  ■••  ^ 

t  Richard  Hakluyt  rode  two  hundred  milea  to  hear  the  Narrative' 
of  Mr.  Thomas  Butt's  Voyage,  temp.  Henry  VIII.  from  England  to 
Newfoundland.— Hakluyt,  partiii,  p.  131. 


%. 


.^-#* 


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t 


\ 


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""!»« 


# 


"m 


«,? 


■^  J.. 


*.;■■ 


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■«i 


•.*P'\^V7'WTOWSW|BpU'**'*hV,jlljA(Mi 


■  «f 


32 


ON  APPROACHIirO 


ji 


I 

I   4 


.  s 


.* 


The  19th  of  these  queries,  is  the  following  :— 
**  How  near  any  one  hath  been  known  to  approach 
the  Pole?" 

^  Answer.  "I  once  met,  upon  the  Coast  of  Green- 
land, a  Hollander,  that  swore  he  had  been  but  half 
a  degree  from  the  Pole,  showing  me  his  Journal, 
which  was  also  attested  hj  his  mate;  m^iere  they  had 
seen  no  ice  or  land,  but  all  water/** 
After  which  Mr.  Oldenburgh  adds,  as  from  himself, 

•♦Thi8isincredible."t 

It  may  not  be  improper,  therefore,  after  mentioning 
this  first  instance  of  a  navigator's  having  approached 
so  near  to  the  Pole,  to  discuss  upon  what  reasons 
Mr.  Oldenburgh  might  found  his  very  peremptory 
incredulity.  -^ 


*  Mr.  Boyle  mentions  a  similar  account,  which  he  received  from 
an  old  Greenland  Master,  on  the  6th  of  April,  1676. — See  Boylels 
Works,  vol.  ii.  p.  397  to  399,  folio.  The  whole  of  this  Narrative 
is  very  circumstantial,  and  deserves  to  be  stated  at  length.  The 
title  is  "  Experiments  and  Observations  made  in  December  and 
January,  1662."  ,„ 

t  See  Dr.  Birch's  History  of  the  Royal  Society,  vol.  I.  p.  202. 
These  queries  are  nineteen  in  number,  to  which  the  answers  are 
very  circumstantial.  I  had  an  opportunity  of  reading  them  over  to 
three  very  inteUigent  masters  of  Greenland  ships,  who  confirmed 
every  particular.  One  circumstance  I  think  it  right  to  take  notice 
of,  though  it  does  not  immediately  relate  to  the  point  in  discussion, 
which  is,  that  there  are  coals  in  Spitzbei^en,  by  which  seven  of 
Mr.  Grey's  crew  were  enabled  to  bear  the  seventy  of  the  winter, 
having  been  left  behind  by  an  accident.  One  of  the  Greenland 
Masters,  to  whom  I  read  Mr.  Grey's  answers,  confirmed  this  par- 
ticular ;  saying,  that  he  had  burnt  himself  SpitEben;cn  r,oa!«,  and 
that  they  were  very  good. 


■ 

p  " 
^ 

■^  -letfT 

■■*"^-*  ?-. 

../■ 


«»**«« 


THl!  NORTH  POLE. 


approach 

ofGreen- 

1  but  half 

Journal, 

they  had 

n  himself, 

lentioning 
>proachtid 
it  reasons 
eremptory 


eceived  from 
-See  Boyle*8 
bis  Narrative 
ength.  The 
ecember  and 

1.  I.  p.  202. 
answers  are 
them  over  to 
ho  confirmed 
o  take  notice 
in  discussion, 
ich  seven  of 
f  the  winter, 
te  Greenland 
tned  this  par- 
tn  coals,  an<l 


tTas  it  because  the  fact  is  impossible  upon  the 
rery  stating  it  ? 

This  puts  me  in  mind  of  the  disbelief  nvhich  is 
generally  shown  to  a  passage  in  Pliny,  even  after  th^ 
actual  f^ct  hath  shown  not  only  the  possibility,  but 
easy  practicability  of  what  is  alluded  to.  Pliny  in^^ 
forms  Uo/  that  Eudoxus,  flying  the  vengeance  of  king 
Lathyrus,  sailed  from  AraUa,  and  reached  the  Straits 
of  Gibraltar :  yet  no  one  scarcely  will  believe  this 
account  of  Edoxus^s  navigation,  notwithstanding  this 
course  is  so  often  followed. 

Was  it  because  no  Englishman  had  then  been  so 
far  to  the  Northward?  .•     -  .    i^^         '  *   ' 

It  is  very  easy,  however,  to  account  why  such 
attempts  should  rather  be  made  by  the  Dutch  than 
the  English  in  the  infancy  of  the  Greenland  Fishery. 

The  southern  parts  of  this  country  were  discovered 
by  Sir  Hugh  Willougbby,  A.  D.  1553 ;  after  which  no 
English  ships  were  sent  on  that  coast  for  nearly  fifty 
years.  In  the  beginning  of  the  last  century,  however, 
a  competition  arose  between  the  English  and  Dutch 
with  regard  to  the  Whale  Fishery,  and  the  English 
drove  the  Dutch  from  most  of  the  harbours,  under 
the  right  of  first  discoverers,t  in  which  they  were^ 

•  Lib.  ii.  chap.  Ixvii. 

t  It  is  also  assigned,  in  the  Supplement  to  Wood  and  Marten's' 
Voyages,  p.  179,  8vo.  1694,  as  a  reason  why  the  English  never 
proceeded  farther  than  78°  on  the  East  Coast  of  Spitzbergen,  because 
the  Dutch  were  commonly  superior  on  that  side  of  the  Island. 

Robert  Bacon,  of  Crowmers  in  Norfolk,  was  the  first  discoverer 
also  of  Iceland. — See  the  Itinerary  of  William  of  Worcester,  p.  31 1. 
8vo.  Cambridge,  1778. 

5 


.# 


i 


^•' 


'*.  ^ 


,n^ 


-^>* 

.■'t^ 


■*l^; 


!^' 


.J 


* 


'ft 


i-^ 


.«•■ 


# 


*.  -. 


■••S^.V--..   *A^- 


»^t 


'{•I  UN  APPHUACIIINA     C  , 

Hupported  by  royal  instructions ;  so  that  the  Dutch 
were  obliged  to  ueek  for  new  stations,  whereas  the 
English  were  commonly  in  possession  of  the  Green- 
land Ports,  which  they  considered  as  their  own.* 
.^  Did  Mr.  Oldenburgh  disbelieve  the  Dutchman's 
relation,  because  ice  is  frequently  met  with  to  the 
Southward  of  North  latitude  80^^ 

Ice  is  commonly  seen  upon  the  great  bank  of  New- 
foundland, and  the  harbour  of  Louisburgh  is  oflen 
covered  with  it,  which  is  only  in  North  latitude  46"* ; 
yet  Davis  and  Baffin  have  penetrated,  under  nearly 
the  same  meridians,  beyond  70". 

I  will  now  suppose  the  tables  changed  between  the 
two  hemispheres  of  our  globe,  and  that  a  Southern 
discoverer,  meeting  with  ice  upon  the  banks  of  New- 
foundland, returns  to  his  own  hemisphere  fully  im- 
pressed with  the  impossibility  of  proceeding  much  to 
the  Northward  of  North  latitude  46° ;  would  not  his 
countrymen  be  deceived  by  the  inferences  which 
were  drawn  from  what  had  been  observed  in  the  seas 
of  the  Northern  hemisphere  ? 

j  Bouvet,  in  1738,  sailed  to  53"  Southern  latitude, 
and  in  a  meridian  5°  to  the  West  of  the  Cape  of  Good 
Hope,  in  which  situation  he  fell  in  with  floating  ice ; 
after  which  he  did  not  proceed  any  farther.  Our 
two  sliips  of  war,  lately  sent  upon  discoveries  to  the 
Southward,  however,  have  been  some  minutes  within 


w- 


'*^-,^;; 


*  See  Purchas,  passiin.  Wliilst  these  disputes  continued,  the 
Dutch  often  sent  ships  of  war  to  protect  their  Greenland  traders, 
which  accounts  for  Dr.  Dallie's  saiUng  in  such  a  vessel  to  86°^  as  I 
have  stated  in  my  former  Paper.  >-.!, 


h 


.rp 


■t- 


^^ 


■^■«  «n>.tt.a  - 


•d*'-"S?s6!*~- 


'^^•' 


I  r 


e  Dutch 
reas  the 
Greeii- 
iwn.* 
tchman^s 
1  to  the 

of  New- 
is  oflen 

tude46'; 

er  nearly 

;ween  the 
Southern 
3of  New- 
!  fully  im- 
r  much  to 
Id  not  his 
es  which 
a  the  seas 

I  latitude, 
e  of  Good 
ating  ice ; 
[ler.  Our 
ies  to  the 
tes  within 


ntinued,  the 
and  traders, 
to  88°,  as  1 


Mf 


THE  NORTH  POLE. 


tHe  Antarctic  Circle,  upon  a  no  very  distant  meridian 
from  that  in  wliich  Bouvct  sailed.  > 

Must  the  fact  be  disbelieved  because  all  the  ice  in 
the  Polar  seas  comes  from  the  Northward  ?  But  this 
is  not  so,  as  Mr.  Grey  informs  us,*  that  the  South- 
east wind  brings  the  greatest  quantity  of  ice  to  the 
coasts  of  Spitzbergcn;  wliich  indeed  is  highly  proba- 
ble, as  this  wind  blows  from  those  parts  of  the  ley 
sea  into  which  the  great  rivers  of  Siberia  and  Tar- 
tary  empty  themselves.f  My  own  poor  conception, 
with  regard  to  the  floating  ice  .  in  the  Spitzbergcn 
seas,  is,  that  these  masses  come  almost  entirely 
from  the  same  quarter,  as  it  is  so  difficult  to  freeze 
any  large  quantity  of  salt  water.  These  pieces  of 
ice,  therefore,  being  once  launched  into  the  Icy 
Sea,  are  dispersed  by  winds,  tides,  and  currents,  in 
every  direction,  some  of  them  being  perhaps  carried 
to  very  high  Northern  latitudes,  from  which  they  are 
again  wafted  to  the  Southward. 

But  allowing,  for  an  instant,  that  all  the  ice  mrty 
come  from  the  Northward,  must  not  then  an  opr '•  xea 
be  left  in  the  higher  Northern  latitudes,  froiii  \Miich 
these  masses  of  ice  are  supposed  to  have  floated  ? 

Was  it  because  the  more  one  advances  towards 
the  Pole,  vegetation  invariably  is  diminished  ? — But 
this  is  not  the  fact. 

*  Dr.  Birch's  History  of  the  Royal  Society. 

t  The  ice  is  said  to  be  never  troublesome  in  the  harbour  of  New- 
port (Rhode-Island,  North  America  ;)  because  no  fresh  water  rivers 
empty  themselves  by  this  port ;  whereas  the  harbour  of  New-York 
(though  much  to  the  southward)  is  often  obstructed  by  the  ice, 
tvhich  floats  down  from  Hudson's  river. 


V.-at 


^? 


^ 


%: 


^ 


■% 


••#' 


# 


.Oix 


■*f.  ■. 


if 


# 


^* 


i¥»» 


Q|l  M>P|10ACIIIK9 

.J.  w 


Nova  Zembla,  situate  only  in  North  latitude  76*, 
produces  not  even  any  sorts  of  grass  ;*  eo  that  the 
only  quadrupeds  which  frequent  it  are  foxes  and  hears, 
>^  l)oth  of  which  are  carnivorous.  In  the  Northern 
>  parts  of  Spitzhergen,  on  the  other  hand,  they  have 
reindeer,  which  are  often  ei^cessively  fat;  and  Mr, 
Grey  mentions  three  or  four  plants,  which  flower 
there  during  the  suimner.f 

Was  it  because  no  one  had  ever  conceived  it  pos- 
sible to  proceed  so  far  as  the  Pole  ?J 

Thome,  however,  a  merchant  of  Bristol,  had  made 
such  a  proposal  in  the  reign  of  Henry  V III ;  and  I 
shall  now  also  show,  that  not  only  Mr.  Oldenburgh*^ 
contemporaries  continued  to  believe  such  a  voyage 
to  be  feasible,  but  many  great  names  in  science  who 
lived  after  him. 

Wood  sailed  on  the  discovery  of  a  Northeast  pas-* 
sage  to  Japan  in  1676;  and,  in  the  publication  of  hia 
yoyage,  he  hath  stated  the  grounds  upon  which  he 
ponceived  such  a  voyage  to  be  practicable;  the 
strongest  of  all  which,  perhaps,  is  the  relation  of 
C/aptain  Goulden,  with  regard  taa  Dutch  ship  having 
reached  North  latitude  89^  Though  this  account 
{lath  often  been  referred  to,  I  do  not  recollect  to  have 
seen  it  stf^ted  with  all  the  circumstanced  which  seem 

•  '■'    -■     '--  ■  -it:- 

#  Purchas,  vol.  i.  p.  479. 

t  Dr.  Birch's  History  of  the  Royal  Society,  vol.  i.  etteq^. 

I  A  Map  of  the  Northern  Hemisphere,  published  at  Berlin  (under 
the  direction  of  the  Academy  of  Sciences  and  Belles  Letters,)  places 
a  ship  at  the  Pole,  as  having  arrived  tl^ere  according  to  ihfi  Dut^ h 
f^ccounts. 


* 


■*  ♦■•        if' .A 


ft'"' 


»     ^fv^*; 


%*,  ^^4 


THE  NORTH  POLS. 


"•Wv, 


ude  76*, 
that  the 
id  hears, 
Northern 
ley  have 
and  Mr, 
flowey 

d  itposi- 

lad  made 
I;  and  I 
nburgh'i} 
I  voyage 
ince  vvho 

east  pas'^ 
ionof  hi& 
ivhich  he 
ble;  the 
Nation  of 
ip  having 
account 
it  to  have 
Ich  seen) 


irlin  (under 

ers,)  places 

^e  Dutfph 


to  establish  its  veracity  beyond  contradiction :  I  shall ; 
therefore  copy  the  very  words  of  Wood.* 

"Captain  Goulden,  who  had  made  above  thirty 
voyages  to  Greenland,  did  relate  to  His  Majesty, 
that,  being  at  Greenland  some  twenty  years  before, 
he  was  in  company  with  two  Hollanders  to  the  east- 
ward of  Edge's  Island  :t  and  that  the  whales  not 
appearing  on  the  shore,  the  two  Hollanders  were 
determined  to  go  farther  Northward,  and  in  a  fort- 
night's time  returned,  and  gave  it  out  that  they  had 
sailed  into  the  latitude  89%  and  that  they  did  not 
meet  with  any  ice,  but  a  free  and  open  sea ;  and  that 
there  run  a  very  hollow  grownX  sea,  like  that  of  the 
Bay  of  Biscay.  Mr.  Goulden  being  not  satisfied  with 
the  bare  relation,  they  produced  him  four  Journals 
put  of  the  two  ships,  which  testified  the  same,  and 
that  they  all  agreed  within  four  minutes.''§ 

*  Moxon's  account  of  a  Dutch  ship  having  been  two  degrees  be» 
yoiid  the  Pole  was  also  much  relied  upon  by  Wood,  which  hath 
never  been  printed  at  large,  but  in  a  now  very  scarce  tract  of  Mox- 
pn's,  and  in  the  second  volume  of  Harris's  Voyages,  p.  396.  In 
confirmation  of  this  very  circumstancial  and  interesting  narrative,  I 
have  only  to  add,  that  Moxon  was  hydrographer  to  Chnrles  II.  and 
hath  published  several  scientific  treatises. — See  the  Catalogue  of 
the  Bodleian  Library.  iy,:,  ► 

t  Edge's  Island  was  discovered,  A.  D.  1616,  by  Captain  Thomas 
Edge,  who  had  made  ten  voyages  to  those  seas. — See  the  Supple- 
ment to  the  Northeast  Voyages,  8vo.  London,  1694.  Whyche'a 
Island,  so  called  from  a  gentleman  of  that  name,  was  discovered  in 
the  following  year. — Ibid.  '  r 

I  Grown  Sea,  is  the  expression  in  the  original.  "  Which  is  not 
practicable  in  these  tempestuous  high^^rown  seas." — Dr.  Hidley,  ia 
his  Journal,  p.  45. 

§  Wood's  Voyage,  p.  145. — Wood's  Voyage  was  published  by 
Smith  and  Walford,  Printers  to  the  Royal  Society  in  1694,  together 


'^ 


.f 


L  ' 


38 


i  ON  APPROACHING 


't 


4/ I 

:-0 


Having  thus  stated  Wood's  own  words,  it  should 
seem,  that  they  who  deny  the  authenticity  of  the 
relation  must  contend,  that  the  crews  of  both  these 
Dutch  ships  entered  into  a  deliberate  scheme  of 
imposing  upon  their  brother  Whale  Fishers,  and  had 
drawn  up  four  fictitious  Journals  accordingly,  because 
so  many  are  stated  to  have  been  produced  out  of  the 
two  ships  to  Captain  Goulden,  whilst  each  of  them 
varied  a  few  minutes  in  the  latitude ;  whereas,  if  they 
had  determined  to  deceive  Captain  Goulden  and  his 
crew,  the  Journals  would  probably  have  tallied  ex- 
actly. I  must  beg  leave  also  to  make  additional 
observation  on  the  account  as  stated  by  Wood,  which 
is,  that  the  Dutch  ships  only  went  to  the  Northward, 
in  search  of  whales,  but  did  not  give  it  out  that  they 
intended  to  make  for  the  Pole,  which,  if  they  had 
done,  it  might  possibly  have  been  an  inducement  to 
carry  on  the  deception  by  forgeries  and  misrepre- 
sentations. To  this  it  may  likewise  be  added,  that 
the  Dutch  are  not  conmionly  jokers. 

I  have  already  remarked,  that  Wood  makes  this 
account  one  of  the  principal  reasons  for  his  undertak- 
ing the  Northeast  passage  to  Japan.  Wood  therefore 
(Mr.  Oldenburgh's  contemporary)  was  not  a  disbe- 
liever before  his  voyage,  of  the  possibility  of  reach- 
ing so  high  a  Northern  latitude,  nor  of  any  of  the  cir- 
cumstances stated  in  this  Narrative. 

But  Captain  Wood  is  not  a  single  instance  of  such 
credulity,  as,  the  very  year  before  he  sailed  on  his 

with  Sir  John  Narborough's,  Marten's,  and  other  Navigators .  The 
book  is  dedicated  to  Pepys,  Secretary  to  the  Admiralty ;  and  he  i« 
complimented  therein  for  having  furnished  the  materiali?. 


/ 


* 


THE  NORTH  POLE. 


39 


t  should 

'  of  the 

h  these 

leme  of 

and  had 

because 

\i  of  the 

of  them 

,  if  thej 

I  and  his 

Jlied  ex- 

dditional 

d,  which 

rthward, 

hat  they 

hey  had 

ement  to 

nisrepre- 

led,  that 

akes  this 
ndertak- 
iherefore 
a  disbe- 
►f  reach- 
f  the  cir- 

of  such 
id  on  his 

on.    The 
and  he  is 


voyage,  we  find  in  the  Philosophical  Transactions  for 
1675*  the  following  passage: — "For  it  is  well  known 
to  all  that  sail  Northward,  that  most  of  the  Northern 
coasts  are  frozen  up  many  leagues,  though  in  the 
open  sea  it  is  not  so,  «o,  nor  under  the  Pole  itself^  unless 
by  accident."  In  which  passage,  the  having  reached 
the  Pole  is  alluded  to  as  a  known  fact,  and  stated  as 
such  to  the  Royal  Society. 

Wood  indeed,  after  i.jt  being  able  to  proceed 
iarther  than  North  latitude  76°,  discredits  in  the  lump 
all  the  former  instances  of  having  reached  high 
Northern  latitudes,  in  the  following  words : — 

"  So  here  the  opinion  of  William  Barentz  was  con- 
futed, and  all  the  Dutch  relations,t  which  certainly 
are  all  forged  and  abusive  pamphlets,  as  also  the 
relations  of  our  countrymen."^ 

Injustice,  however,  to  the  memoirs  of  both  English 
and  Dutch  Navigators,  I  cannot  but  take  notice  of 
these  very  peremptory  and  ill-founded  reflections, 
made  by  Wood:  and  which  seem  to  be  dictated 
merely  by  his  disappointment,  in  not  being  able  to 
effect  his  discovery. 

Wood  attempted  to  sail  in  a  Northeast  direction 
between  Spitzbergen  and  Nova  Zembla,  but  was 
obstructed  by  ice,  so  that  he  could  not  proceed 
farther  than  the  West  coast  of  Nova  Zembla,  in  North 

*  No.  118. 

t  The  Dutch  made  three  voyages  for  the  discovery  of  the  North- 
east Passage  in  three  successive  years,  the  thirJ  being  in  1596, 
which  last  was  by  the  encouragement  of  a  private  subscription  only. 
— See  Gerard  de  Veer,  p.  13.  folio.  Amsterdam,  1609. 

J  Wood's  Voyage,  p.  181. 


'■  -3»  _H, 


•5v. 


■.f  %. 


■*^w 


40 


ON  APPROACHING 


J¥*' 


I 


h 


latitude  76*.  Thinking  it,  therefore,  prudent  to 
return,  he  at  once  treats  as  fabulous,  not  only  the 
ideas  of  that  most  persevering  seaman,  William 
Barentz,  but  likewise  all  other  accounts  of  ships 
having  ireached  high  Northern  latitudes.  Now  that 
the  ice,  which  obstructed  Wood  in  North  Latitude 
76",  was  not  a  perpetufil,  but  only  an  occasional  bar- 
rier, appears  by  the  Russians  having  not  only  dis- 
covered, but  lived  several  years  in  the  island  of 
Maloy  Brun,  which  lies  between  Spitzbergen  and 
Nova  Zcmbia,  and  extends  from  North  latitude 
77"  25'  ^o  TS**  45*  The  Dutch  also  sailed  round  the 
Northern  Coast  of  Nova  Zembla,  and  wintered  on  the 
Eastern  side  in  1596.t  if*' 

As  for  Wood's  treating  all  discoveries  towards  the 
Pole,  from  the  Northern  parts  of  Spitzbergen,  as 
fabulous,  he  had  not  the  least  foundation,  from  what 
he  had  observed  on  his  own  voyage,  for  this  un- 
merited aspersion  upon  their  veracity;  because,  if 


I, 


*  See  the  English  Translation  of  Professor  Le  Roy's  account  of 
this  Island,  p.  85,  8vo.,  London,  1774,  printed  for  C.  Heydinger. 
As  also  the  Sieur  de  Vaugondy'sJSjsai  d'une  Carte  Polaire  Arctique, 
published  in  1774,  who  represents  this  Island  as  extending  from 
North  latitude  77»  20'  to  78«»  3(/,  its  longitude  being  60"  East  from 
Fero. 

t  See  the  Map  of  the  circumpolar  regions,  which  accompanies 
Wood's  Voyage.  The  Northern  point  of  Nova  Zembla,  in  this  Map, 
is  in  77®  nearly.  There  were  factions  in  Holland  with  regard  to 
the  method  of  discovering  the  Northeast  Passage.  Barentz,  insti- 
gated  by  Plancius,  the  geographer,  was  for  making  the  trial  to  the 
North  of  Nova  Zembla ;  the  other  two  ships,  which  sailed  on  that 
expedition  of  discovery,  were  to  attempt  passing  the  Weygatz.— 
Recueil  dee  Voyages  au  Nord.  torn.  iv.    Linachoteu's  Preface. 


^ 


^ 


•v,.-a^,m;  ^#., 


Tlf£  NORTH  POLE. 


41 


ident  to 
only  the 
William 
of  ships 
ow  that 
Latitude 
>nal  bar- 
only  dis- 
sland  of 
•gen  and 
latitude 
'ound  the 
ed  on  the 
*■ 
rards  the 
ergen,  as 
rom  what 
this  un- 
;cause,  if 


account  of 
Heydinger. 
re  Antique, 
inding  from 
°  East  from 

ccompanies 
in  this  Map, 
i  regard  to 
entz,  insti- 
trial  to  the 
[led  on  that 
tVeygatz.— 
'reface. 


Wood's  barrier  between  Spitzbergen  and  Nova 
Zambia,  in  North  latitude  76%  had  been  perpetual, 
what  hath  this  to  do  with  the  course  of  a  ship  sailing 
from  the  Northern  parts  of  Spitzbergen  upon  a  me- 
ridian towards  the  Pole  ? 

I  cannot,  however,  dismiss  Wood's  Voyage  without, 
making  some  further  remarks  on  his  concluding,  that 
the  obstructions  which  he  met  with  in  North  lati- 
tude 76*  were  perpetual. 

Almost  every  voyage  to  seas  in  which  floating  ice 
is  commonly  to  be  found,  proves  the  great  diflTerence 
between  the  quantities,  as  well  as  size,  of  these 
impediments  to  navigation,  though  in  the  same  lati- 
tude and  time  of  the  year. 

Davis,  in  his  two  first  voyages  to  discover  the 
Northwest  Passage,  could  not  penetrate  beyond 
66";  but  in  his  third  voyage,  in  1587,  he  reached 
72"  12'.* 

In  the  year  1576,  Sir  Martin  Frobisher  passed  the 
Straits  (since  called  from  their  first  discoverer) 
without  any  obstructions  from  ice;  in  his  two  fol- 
lowing voyages,  however,  he  found  them  in  the  same 
month,  to  use  his  own  expression,  "  in  a  manner  shut 
up  with  a  long  mure  of  ice."t 

In  the  year  1614,  Baffin  proceeded  to  81",  and 
thought  he  saw  land  as  far  as  82'!  to  the  Northeast 
of  Spitzbergen,  which  is  accordingly  marked  in  one 

*  See  Hakluyt,  and  Purchas,  vol.  i.  p.  84.  '  •     • 

t  Purchas,  ibid. 

J  See  also  the  Supplement  to  Wood  and  Marten's  Voyages,  in  the 
tvo.  publication  of  1694,  in  which  Point  Purchas  ,i8  stated  to  be  in 
North  Latitude  SS". 

6 


M. 


^>« 


%: 


42 


H 


ON  ArPROACHlN« 


•*• 


* 


of  Purchas's  Maps.  During  this  voyage  he  met,  near 
Cherry  Island,  situate  only  in  74"  North  latitude, 
two  banks  of  ice;  the  one  forty  leagues  in  length, 
the  other  one  hundred  and  twenty ;  which  last  would 
extend  to  twenty-five  degrees  of  longitude  in  North 
latitude  76%  where  Wood  fixes  his  barrier. 

It  need  therefore  scarcely  be  observed,  that  such 
a  floating  wall  of  ice,  one  hundred  and  twenty 
leagues  long,  by  being  jammed  in  between  land,  or 
other  banks  of  ice,  might  afford  an  appearance 
indeed  of  forming  a  perpetual  barrier,  when,  perhaps, 
w'*hin  the  next  twenty-four  hours,  the  wall  of  ice 
might  entirely  vanish. 

Of  the  sudden  assemblage  of  such  an  accumula- 
tion of  ice,  I  shall  now  mention  two,  rather  recent, 
instances. 

I  have  been  very  accurately  informed,  that  the 
late  Colonel  Murray  happened  to  go,  in  the  month  of 
May,  from  one  of  our  Southern  Colonies  to  Louis- 
burgh,  when  the  harbour  was  entirely  open ;  but,  on 
rising  in  the  morning,  it  was  completely  filled  with 
ice,  so  that  a  wagon  might  have  passed  over  it  in 
any  direction.* 


Ih 

office 


■«..  ^ 


*  On  the  19th  of  December,  1769,  the  Potowmack,  in  a  part 
where  it  was  two  miles  broad,  and  nearly  in  North  Latitude  of  only 
38°,  was  frozen  entirely  over  in  one  night,  when  the  preceding  day 
had  been  very  mild  and  temperate. — Burnaby'a  Travels  through 
North  America,  p.  59. 

Camden,  in  his  Annals  of  Elizabeth,  asserts,  that  Davis  reached 
83°,  where  the  Straits,  called  after  him,  were  narrowed  to  forty 
leagues.— See  Camden,  anno  1585.  We  have  oot  since  been  able 
to  proceed  so  far  to  the  Northward.  , . 


>f*' 


THE  NORTH  POLE. 


43 


le  met,  near 
th  latitude, 
i  in  length, 
i  last  would 
e  in  North 
r. 

[,  that  such 
md  twenty 
en  land,  or 
ippearancc 
n,  perhaps, 
ivall  of  ice 

accumula- 
ler  recent, 

I,  that  the 
e  month  of 
to  Louis- 
n ;  but,  on 
filled  with 
over  it  in 


«,  in  a  part 
tude  of  only 
receding  day 
'els  through 

avis  reached 
red  to  forty 
:c  been  able 


I  have  also  received  the  following  account  from  an 
officer  in  the  Royal  Navy,  who  was  not  many  years 
ago  on  the  Newfoundland  station. 

In  the  middle  of  June  the  whole  Straits  of  Bellisle 
were  covered  in  the  same  manner  with  the  harbour 
of  Louisburgh,  and  for  three  weeks  together  a  car- 
riage might  have  passed  from  one  shore  to  the  other ; 
but  during  a  single  night  the  ice  had  almost  entirely 
disappeared.  Such  is  the  sudden  accumulation  of 
ice,  in  latitudes  twenty-four  and  thirty  degrees  to  the 
Southward  of  Wood's  situation. 

Linschoten  asserts,  that  being  in  the  Straits  of 
Weygate,  the  last  day  of  July,  he  was  told  by  the 
Samoieds  on  that  coast,  that  in  ten  or  twelve  days 
afterward  the  ice  in  the  Straits  would  be  all  gone, 
though  they  were  then  quite  blocked  up  with  it. 
When  he  repassed  these  Straits  afterward,  on  the 
13th  of  August,  he  found  not  the  least  vestige  of  it, 
so  quickly  do  these  huge  masses  dissolve  after  they 
once  begin  to  thaw.* 

On  the  other  hand,  Callander  admits,  that  by 
accumulation  of  floating  ice  places  are  now  inacces- 
sible which  were  not  formerly  so,  and  instances  the 
Eastern  Coast  of  Greenland,  as  also  Frobisher's 
Straits.f  Kergulen,  in  his  account  of  Iceland,  like- 
wise mentions,  that  the  sea  between  Iceland  and 
Greenland  was  entirely  closed  during  the  whole 
summer  of  1766. 

I  shall  now  endeavour  to  show,  that  Dr.  Halley 
was  no  more  incredulous  with  regard  to  the  pos- 
sibility of  reaching  high  Northern  latitudes,   than 

*  Callander's  Preface,  p.  38.  t  Ibid. 


««#;.  J 


•   % 


#^ 


■  *  ».. 


■f 


W' 


ON  APPROACHING 


<«! 


Captain  Wood  was  before  the  ill  success   of  his 
voyage  on  discovery. 

Mr.  Miller,  in  his  Gardener's  Dictionary,  hath  the 
following  passage,  under  the  article  Thermometer  : — 

"  Mr.  Patrick  has  fixed  his  thermometer  to  a  scale 
of  90%  which  are  numbered  from  the  top  downward, 
and  also  a  moveable  index  to  it.  The  design  of  this 
is  to  show,  how  the  heat  and  cold  is  changed  from 
the  time  it  was  last  looked  upon,  according  to  the 
difTerent  degrees  of  heat  and  cold  in  all  latitudes. 
As  by  the  trial  of  two  thermometers,  which  have  been 
regulated  abroad ;  the  one  by  Dr.  Halley,  in  his  late 
Southern  oyage ;  and  the  other  by  Captain  Johnson, 
in  his  voyage  to  Greenland;  the  first  hath  a  hest 
under  the  equinoctial  line,  and  the  other  a  degree  of 
cold  in  88°  of  North  latitude." 

I  have  taken  some  pains  to  find  out  a  more  full 
account  of  tljis  voyage  of  Captain  Johnson's;  but 
have  only  met  with  the  following  confirmation  of  it 
perhaps : — 

"  I  have  been  assured,  by^persons  of  credit^  that  an 
English  Captain,  whose  name  was  Monson,  instead 
of  seeking  a  passage  to  China  between  the  Northern 
countries,  had  directed  his  course  to  the  Pole,  and 
had  approached  it  within  two  degrees,  where  there 
was  an  open  sea,  without  any  ice."* 

As  the  Captain  Monson  mentioned  in  this  passage, 
reached  exactly  the  same  degree  of  latitude  with 
Captain  Johnson,  I  should  rather  think,  that  this  is 
the  same  voyage;  especially,  as  it  is  well  known, 


*  See  M.  de  Buflfon's  Natural  History,  vol.  i,  p.  216.  4to, 


% 


THE  WORTH  POLE. 


•4. 


IS 


8  of  his 
hath  the 

METER :— 

0  a  scale 
jwnward, 
;n  of  this 
iged  from 
)g  to  the 
latitudes, 
have  been 
n  his  late 
Johnson, 
h  a  heat 
iegree  of 


nore  full 
n's ;  hut 
ion  of  it 


)  that  an 
,  instead 
Vorthern 
ole,  and 
re  there 

passage, 

ide  with 

t  this  is 

known, 

Ito, 


H'    «", 


that  the  French  writers  seldom  trouble  themselves 
about  the  orthography  of  foreign  names. 

If  this,  however,  should  not  be  the  case,  it  must 
be  admitted  to  be  ua  additional  instance  of  a  ship's 
leaving  reached  North  latitude  88°,  as  well  as  Mons. 
de  Buffbn's  giving  credit  to  such  relation.* 

Having  therefore  not  been  able  to  pick  up  any 
other  circumstances  in  relation  to  Captain  John- 
son's voyage,  I  shall  now  state  what  seems  to  be  fairly 
deducible  from  the  passage,  which  I  have  copied 
from  Miller's  Gardener's  Dictionary. 

Dr.  Halley  made  his  voyage  to  the  Southward  in 
1700;  on  the  return  from  which,  he  probably  em- 
ployed Patrick,  as  the  most  eminent  maker  of  weather 
glas8e8,t  to  ^-c  Juate  a  thermometer  according  to  the 
heat  he  had  experienced  under  the  equator.  It  was 
very  natural,  therefore,  when  such  a  point  of  heat 
was  to  be  marked  upon  the  instrument,  to  make  the 
scale  either  for  high  Southern  or  Northern  latitudes. 

It  should  seem,  then,  that  Dr.  Halley  had  procured 
Captain  Johnson  (who  was  Master  of  a  Greenland 

*  To  this  list  of  credulous  persons  (as  perhaps  they  may  be  con- 
sidered by  some,)  I  shall  beg  leave  to  add  the  names  of  Maclauria 
and  Dr.  Campbell.  The  former  of  these  was  so  persuaded  of  tlie 
seas  being  open  quite  to  the  Pole/  that  he  hath  not  only  advised  this 
method  of  prosecuting  discoveries,  but,  as  I  have  been  told,  was 
desirous  of  going  the  voyage  himself. 

t  I  have  been  informed,  that  his  shop  was  in  the  Old  Bailey,  and 
that  he  died  about  fifty  years  ago.  Patrick  was  a  great  ringer,  and 
some  of  the  most  celebrated  peals  were  invented  by  him,  more  than 
fifty  years  ago.  He  styled  himself,  in  tiis  advertisements,  Torri- 
cellian Operator. — Sir  John  Hawkins's  History  of  Music,  vol.  iv. 
p.  154. 


^1 


f 


■It' 


V 


>'. 


/ 


\ 


tu 


4 


46 


J!^t 


•rr  APPROACHINO 


ship)  to  carry  a  thermometer  on  his  voyage  to  Spitz- 
bergen,  and  that  he  fortunately  was  able  to  reach  so 
high  a  degree  of  latitude  as  88°. 

If  the  thermometer  had  been  calculated  only  for 
imaginary  degrees  of  heat  and  cold,  it  would  have 
been  marked  for  the  Equator  and  the  Pole ;  whereas 
it  was  only  regulatad  for  88"  of  North  latitude,  which 
Captain  Johnson  therefore  had  as  clearly  reached^ 
as  Dr.  Halley  had  the  Equator. 

At  all  events,  Patrick's  Thermometer  must  have 
been  made  under  Dr.  Halley's  inspection ;  and  would 
he  have  permitted  it  to  be  marked  for  88*  of  North 
latitude,  according  to  Captain  Johnson's  voyage,  if 
he  had  disbelieved  his  narrative  ? 

My  third  and  last  instance,  from  any  printed 
authority,  but  in  a  book  which  is  not  commonly  to  be 
met  with,  is  that  of  Captain  Alexander  Cluny,  as  by 
a  map  engraved  under  his  direction,  the  very  spot  is 
marked  to  the  Westward  of  Spitzbergen,  and  in 
somewhat  more  than  82°  of  North  latitude,  where  he 
saw  neither  land  nor  ice.* 

Before  I  proceed,  however,  to  state  several  other 
instances  of  reaching  high  northern  latitudes,  which 
have  never  appeared  in  print,  and  which  I  have  col- 
lected since  my  last  Paper  on  this  head,  I  must  beg 
the  indulgence  of  the  Society,  whilst  I  lay  before 


r 


*  Sec  the  American  Traveller,  4to.  London  1769;  as  also,  the 
Sieur  de  Vaugondy's  Essai  d'une  Carte  Polaire  Antique,  published 
in  1774 ;  in  which,  however,  he  lays  down  this  spot  from  Cluny's 
Map,  in  little  more  than  81°,  whereas  it  is  fully  in  82"».  The  lon- 
gitude of  this  spot  is  30«>  East  from  Fero. 


r^ 


m 


THE  NORTH  POLE. 


47 


B  to  Spitz- 
o  reach  so 

>d  only  for 
ould  have 
;  whereas 
ide,  which 
'  reached, 

nust  have 

md  would 

of  North 

voyage,  if 

Y  printed 
only  to  be 
ly,  as  by 
^y  spot  is 
and  in 
where  he 


them  some  additional  reasons  why  the  Polar  Seas 
may  be  conceived  to  be  navigable.* 

Speculative  geographers  have  supposed,  that  there 
should  be  nearly  the  same  quantity  of  land  and  sea 
in  both  hemispheres,  in  order  to  preserve  the  equi- 
librium of  the  globe. 

It  is  possible,  indeed,  that  this  may  be  accounted 
for  by  the  Antarctic  seas  being  more  shallow  than 
those  near  the  North  Pole ;  as  we  do  not  know  this, 
however,  by  the  actual  soundings,  but  are  informed 
by  Captain  Furneaux,  that  there  is  no  land  even  as 
far  as  the  Antartic  Circle,  upon  the  meridian  in  which 
he  sailed,  as  also  that  no  land  was  observed  during 
the  course  of  his  circumnavigation  in  55**  South  lati- 
tude at  a  medium,  it  seems  necessary,  as  the  quan- 
tity of  land  so  greatly  preponderates  in  the  Northera 
hemisphere,  that  from  North  latitude  80^°  to  the  Pole 
itself  must  be  chiefly,  if  not  entirely,  8ea.t 

Let  us  now  consider,  whether  such  a  sea  is  proba- 
ble, at  all  times,  in  a  state  of  congelation. 


ral  other 
8,  which 
lave  col- 
Qust  beg 
y  before 


8  also,  the 
published 

m  Cluny's 
The  Ion- 


r 


*  I  have  received  a  letter  from  the  Rev.  Mr.  Tookc,  Chaplain  to 
the  Factory  at  St.  Petersburgh,  dated  December  30,  1774,  which 
he  concludes  in  the  following  manner : — "  I  have  a  fact  or  two  to 
communicate,  which  seem  to  indicate,  if  not  to  a  certainty,  yet  at 
least  to  a  degree  of  probability,  that  the  sea  is  open  to  the  Pole  the 
year  throughout ;  but  my  paper  will  not  hold  them."  From  the 
accuracy  with  which  several  other  interesting  particulars  are  stated 
in  this  letter,  I  have  great  reason  to  regret,  that  I  have  not  an  op- 
portunity of  laying  the  facts  alluded  to  before  the  Public,  with  all 
their  circumstances,  as  I  suppose  that  Mr.  Tooke's  information 
came  from  Archangel  Seamen. 

t  It  is  not  known  that  Captain  Cook  also  found  very  little  land 
during  his  persevering  attempts  to  the  Southward.  *'' 


■f^ 


'■P^^ 
■'4- 


•t'i 


48 


ON  APPROACHING 


^* 


itf 


I  do  not  know,  whether  it  hath  been  settled  by 
thermometrical  observations,  that  there  is  any  mate- 
rial difTereiice  between  the  heat  under  the  Equator, 
and  that  which  is  experienced  within  the  Tropics ; 
most  travellers  complain  indefinitely  of  its  excess  in 
such  latitudes.  ^  . 

As  this  point,  therefore,  seems  not  to  have  been 
settled  by  the  thermometer,  let  us  have  recourse  to 
what  is  found  to  be  the  freezing  point  upon  mountains, 
situate  almost  under  the  Equator,  and  compare  it 
with  the  same  height  on  the  Peak  of  Teneriffe,  which, 
being  in  North  latitude  28',  is  five  degrees  to  the 
Northward  of  the  Tropical  limits. 

The  French  Academicians  suppose,  that  the 
freezing  point,  at  which  all  vegetation  ceases,  and 
ice  takes  place,  commences  on  Cotopaxi,  at  1411 
toises  above  the  level  of  the  sea ;  or,  by  our  measure, 
at  the  height  of  about  a  mile  and  three  quarters.* 

Mr.  Edens,  on  the  other  hand,  hath  given  us  a  very 
particular  account  of  what  he  observed  in  going  to 
the  top  of  Tenerifie  ;t  and  so  far  from  seeing  snow 
or  ice  (except  in  a  cave)  his  coat  was  covered,  during 
the  night,  with  dew,  at  the  very  summit;  which, 


*  Cotopaxi  is  the  highest  mountain  of  the  Andes,  at  least  in  the 
neighbourhood  of  Quito.  The  plain  of  Carabuca,  from  which  it 
rises,  is  1023  toises  above  the  level  of  the  sea,  and  the  height  of 
the  mountain  above  this  plain  is  1268  toises,  making  together  2291 
toises.  If  880  toises  therefore  are  deducted  from  2291,  141! 
toises  become  the  height  of  the  freezing  point  upon  this  mountain. 
— See  Ulloa's  Account  of  South  America. 

t  Philosophical  Transactions  Abridged,  vol.  v.  p.  147.    Sprat's 
History  of  the  Royal  Society. 


% 


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\. 


.  4 


y.>l/t^li^ 


m 


tied  by 

y  mate- 

iquator, 

Vopics ; 

Lcess  in 

re  been 

)urse  to 

untains, 

fipare  it 
S  which, 

to  the 

hat   the 

ies,  and 

at  1411 

neasure« 

ers.* 

8  a  very 

;oing  to 

ng  snow 

,  during 

which, 

ast  in  the 

1 

1  which  it 

1 

height  of 
ther  2291 

■ 

91,   1411 

mountain. 

.    Sprat*8 

1 

THE  NORTH  POLE. 


i-. 


49 


according  to  Dr.  Heberden^s  computation,  is  l.'),3d6 
feet  high,  or  wants  but  148  yards  of  three  miles.* 

Now,  as  it  is  thus  settled,  that  the  Peak  of  Tene- 
rifTe  is  nearly  three  miles  high,  which  exceeds  by 
more  than  a  mile  the  height  of  the  freezing  point  on 
Cotopaxi,  situate  under  the  Equator,  it  should  seem 
that  there  is  no  particular  diflerenc^  between  the  heat 
under  the  Equator  and  within  the  Tropics ;  for  if  it 
is  urged,  that  Teneriffe  is  more  surrounded  with  sea 
than  Cotopaxi,  it  must  on  the  other  hand  be  recol- 
lected, that  this  mountain  is  situate  5**  to  the  North- 
ward of  the  Tropic,  at  the  same  time  that  the  sum- 
mit exceeds  the  freezing  point  on  Cotopaxi  by  more 
than  a  mile ;  both  which  circumstances  should  ren- 
der it  colder  than  the  freezing  point  on  Cotopaxi. 

The  inference  to  be  drawn  from  this  comparison 
seems  to  be,  that,  as  the  heat  varies  so  little  between 
the  Equator  and  the  Tropical  limits,  it  may  difier  as 
little  between  the  Arctic  Circle  and  the  Pole. 

Nothing  hath  been  supposed  to  show  more  strongly 
the  wisdom  of  a  beneficent  Creator,  than  that  every 
part  of  this  globe  should  (taking  the  year  throughout) 
have  an  equal  proportion  of  the  sun^s  light. 

It  is  admitted,  that  the  equatorial  parts  have  rather 
too  much  heat  for  the  comforts  of  the  inhabitants, 
and  those  within  the  Polar  Circles  too  little ;  but,  as 
we  know  that  the  Tropical  limits  are  peopled,  it 
should  seem  that  the  two  Polar  Circles  are  equally 


*  See  Hawkesworth's  voyages,  vol.  ii.  p.  12.  Goats  also  reach 
the  very  summit,  which  must  be  in  search  of  food,  as  they  do  not 
bear  cold  well. 


v 


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destined  tor  the  same  purpose;  or  if  not  for  the 
benefit  of  man,  at  least  for  the  sustenance  of  certain 
animals. 

The  largest  of  these,  in  the  whcde  seale  of  Crea- 
tion, is  the  whale ;  which,  though  a  fish,  cannot  live 
long  under  water,  without  occasionally  raising  its 
head  into  another  element,  for  the  purpose  of  respi- 
ration :*  most  other  fish  also  occasionally  approach 
^1  the  surface  of  the  water. 

If  the  ice  therefore  extends  from  North  latitude 
b(H**  to  the  Pole,  all  the  intermediate  space  is  denied 
to  the  Spitzbergen  whales,  as  well  perhaps  as  to 
other  fish.  And  is  that  glorious  luminary,  the  sun, 
to  shine  in  vain  for  half  the  year  upon  ten  degrees  of 
latitude  round  each  of  the  Poles,  without  contributing 
either  to  animal  life  or  vegetation?  for  neither  can 
take  place  upon  this  dreary  expanse  of  ice. 

If  this  tract  of  sea  also  is  thus  rendered  improper 
for  the  support  of  whales^,  these  enormous  fish,  which 
require  so  much  room,  will  be  confined  to  two  or 
three  degrees  of  latitude  in  the  neighbourhood  of 
Spitzbergen;  for  all  the  Greenland  Masters  agree, 
^  that  the  best  fishing  stations  are  from  79°  to  80**,  and 
that  they  do  not  often  catch  them  to  the  Southward. 

I  will  now  ask,  iftheseais  congealed  fi*om  North 
latitude  80^**  quite  to  the  Pole,  when  did  it  thus  begin 
to  freeze,  as  it  is  well  kiiown,  that  a  large  quantity  of 


"■*' 


*  "  Sometimes  the  ice  is  ^xed,  when  there  are  but  few  whales 
seen,  for  underneath  the  ice  they  cannot  breathe." — ^Martens's  Voy- 
age to  Spitzbergen. 

The  whales,  likewise,  are  supposed  to  come  from  the  North ,  but 
how  can  thin  be,  if  there  is  an  incrusted  sea  over  them  ? 


^^■ 


/ 


*" 


•fc.:*." 


\  THE  WORTH  POLE. 

sea  water  is  not  easily  forced  to  assume  the  form  of 
ice  ?*  Can  it  be  contended,  that  ten  degrees  of  the 
globe  round  each  Pole  were  covered  with  frozen  sea 
at  the  original  creation  ?t  And  if  this  is  not  insisted 
upon,  can  it  be  supposed,  that,  when  the  surface  of 
the  Polar  Ocean  first  ceased  to  be  liquid,  it  could 
have  afterward  resisted  the  effects  of  winds,  currents, 
and  tides  ?  s 

I  beg  leave  also  to  rely  much  upon  the  necessity  ^ 
of  the  ice^s  yielding  to  the  constant  reciprocation  of 


^:.* 


':f 


.1^ 


*  "  There  are  three  kinds  of  ice  in  the  Northern  Seas.  The 
first  is  like  melted  snow,  which  is  become  partly  hardened,  is 
more  easily  broken  into  pieces,  less  transparent,  is  seldom  more 
than  six  inches  thick,  and,  when  dissolved,  is^und  to  be  intermixed 
with  salt.  This  first  sort  of  ice  is  the  only  one  which  is  ever  formed 
from  sea  water. 

'  "  If  a  certain  quantity  of  water,  which  contains  as  much  salt  as 
sea  water,  is  exposed  to  the  greatest  degree  of  cold,  it  never  becomes 
firm  and  pure  ice,  but  resembles  tallow  or  suet,  whikt  it  preserves  the 
taste  of  salt,  so  that  the  sweet  transparent  ice  can  never  be  formed 
in  the  sea.  If  the  ice  of  the  sea  itself,  therefore,  confined  in  a 
Small  vessel  without  any  motion,  cannot  thus  become  true  ice,  much 
less  can  it  do  so  in  a  deep  and  agitated  ocean."  The  author  hence 
infers,  that  all  the  floating  ice  in  the  Polar  Seas  comes  from  the 
Tartarian  Rivers  and  Greenland,  as  I  have  before  contended. — See 
a  Dissertation  of  Michel  Lomonosof,  translated  from  the  Swedish 
Transactions  of  1752.  Collection  Acadfmtque,  tom.  xi.  p.  5.  et  seq., 
4to.  Paris,  1772.  The  Dissertation  is  entitled,  "Z>e  VOrigim  des 
Monts  de  Olace,  dans  la  Mer  du  J^ord." 

t  If  there  had  been  a  fixed  barrier  of  ice  from  the  time  of  the 
creation,  extending  from  SO^**  to  the  North  Pole,  the  height  of  such 
ice  must  have  been  excessive,  by  the  accumulation  of  frozen  snow 
from  winter  to  winter.  Martens  therefore  observes,  that  the  ice 
mountains  in  Spitzbergen  are  constantly  increasing  by  the  snow  and 

rain  which  falls  freezing,  and  which  seldom  melts  at  the  top.— P.  43. 


.11... 

■4 


?rf. 


t 


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**;; 


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the  latter;  because  no  sea  was  ever  known  to  be 
frozen  but  the  Black  Sea,  and  some  small  parts  of  the 
Baltic,*  neither  of  which  have  any  tides,  at  the  same 
tirae  that  the  waters  of  both  contain  much  less  salt 
than  those  of  other  seas,  from  the  great  influx  of 
many  fresh  water  rivers.  For  this  last  reason,  it  may 
likewise  be  presumed,  that  the  circumpolar  seas  are 
very  salt,  because  there  is  probably  no  such  influx 
beyond  North  latitude  80%  Spitzbergen  itself  having 
no  rivers. 

Having  thus  given  some  general  reeisons,  why  the 
sea  should  not  be  supposed  to  be  frozen  in  the  ten 
highest  degrees  of  latitude,  I  shall  now  proceed  to 
lay  before  the  Society  several  instances,  which  I 
have  lately  collected,  and  which  prove  that  it  is  not 
so  covered  with  ice  considerably  to  the  North  of  8(H^. 

I  shall,  however,  previously  make  two  obsemi^ 
ations ;  the  first  of  which  is,  that  every  instance  of 
exceeding  North  latitude  SOy",  as  much  proves  that 
there  is  no  perpetual  barrier  of  ice  in  that  latitude,  as 
if  the  navigator  hath  reached  the  Pole.  The  second 
is,  that  as  four  experienced  Greenland  Masters 
have  concurred  in  informing  me,  that  they  can  see 
what  is  called  the  bUi^  of  the  ic&\  for  a  degree  before 


4^ 


J 


%> 


*'\' 


*  To  these  perhaps  may  be  added  the  White  Sea. 

t  This  is  described  to  be  an  arch  formt. :  upon  the  clouds  by  re- 
flection from  the  packed  ice.  Where  the  ice  is  fixed  upon  the  sea, 
you  see  a  snow  viaie  brightness  in  the  skies,  as  if  the  sun  shined, 
for  the  snow  is  reflected  by  the  air  just  as  a  fire  by  night  is,  but  at  a 
distance  you  see  the  air  blue  or  blackish.  Where  there  are  many 
small  ice  fields,  which  are  as  meadows  for  the  seals,  you  see  no 
lustre  or  brightness  of  the  skies. — Martens's  Voyage  to  Spitzbergen. 


«jf-jf* 


^^■ 


M 


/' 


m 


■ijsrf  •*■■ 


If 


i«- 


THE  NORTH  1>0LE. 


53 


them,  they  never  can  be  off  Hakluyt's  Headland, 
which  is  situate  in  79'  50',  without  observing  this 
eflect  of  the  ice  upon  the  sky,  if  there  was  a  per- 
petual barrier  at  8(H%  which  is  not  much  more  than 
half  a  degree  from  them,  when  in  that  situation. 
Now  Hakluyt's  Headland  is  what  they  so  perpetually 
take  their  departures  from,  that  it  hath  obtained  the 
name  of  The  Headland  by  way  of  pre-eminence. 

This  mountain  also  is  so  high,  that  it  can  be  dis- 
tinguished at  the  distance  of  a  degree :  in  such 
instances,  therefore,  which  I  shall  produce,  that  do 
not  settle  the  latitude  by  observation,  whenever  the 
reckoning  depends  upon  the  approach  or  departure 
from  this  Headland,  the  account  receives  the  ad- 
ditional check  of  the  mountain's  being  increased  or 
diminished  gradually  to  the  eye  of  the  observer.      '^ 

My  second  previous  remark  shall  be,  with  regard 
to  all  instances  of  reaching  high  Northern  latitudes, 
for  which  the  authority  of  the  Ship's  Journal  may  be 
required,  that  it  is  almost  impossible  to  procure  this 
sort  of  evidence,  except  the  voyages  have  been 
recent ;  not  only  for  the  reasons  I  have  given  in  my 
former  Paper,  but  because  I  find,  that  if  the  Ship's 
Journal  is  not  wanted  b^  the  owners  in  a  year  or  two 
(which  seldom  happens)  it  is  afterward  considered 
as  waste  paper. 

Without  the  least  impeachment  also  of  the  know- 
ledge in  navigation  of  the  Greenland  Masters,  when 
they  are  in  the  actual  pursuit  of  fish,  they  do  not 
trouble  themselves  about  their  longitude  or  latitude ; 
they  are  not  bound  by  their  instructions  to  sail  to  any 
particular  pdlht,  and  their  only  object  is  to  catch  as 


.* 


^, 


m. 


I 


^ 


•^ 


m 


ON  APPROACHING 


V*. 


^nt 


^% 


V,, 


: 
''ink  i 


^'; 


many  whales  as  possible ;  the  ahip^s  situation  there- 
fore, at  such  time,  becomes  a  matter  of  perfect  indif- 
ference. It  will  appear,  however,  that  they  not  only 
keep  their  reckonings,  but  observe,  when  they  are 
not  thus  employed  in  fishing. 

Having  made  these  previous  remarks,  I  shall  now 
proceed  to  lay  before  the  Society  such  instances  of 
navigators  having  penetrated  beyond  BOi%  as  I  have 
happmied  to  procure  since  the  reading  of  my  former 
Paper  on  this  subject,  in  May  last. 

James  Hutton  (then  belonging  to  the  ship  London, 
Captain  Guy)  was,  thirty  years  ago,  in  North  latitude 
8U%  as  both  the  Captain  and  Mate  informed  him ; 
but  did  not  observe  himself.  A  very  intelligent  sea- 
officer  was  so  good  as  to  take  from  him  this  account, 
together  with  the  following  particulars,  which  per- 
haps may  be  interesting  to  Greenland  Navigators. 

Hutton  hath  been  employed  in  the  Whale  Fishery 
nearly  these  forty  years,  during  which  he  hath  been 
several  times  at  the  Seven  Isleinds,  and  the  Waygat 
Straits.  In  some  of  these  voyages  the  sea  hath  been 
perfectly  clear  from  ice,  and  at  other  times  it  hath 
set  in  so  rapidly  towards  the  Waygat,"^  as  to  oblige 
the  vessels  which  happened  to  be  thereabouts  to 
force  all  sail  possible  to  escape  being  inclosed. 

This  hardy  old  tar  likewise  supposes  that  he  hath 
been  farther  up  the  Waygat  than  perhaps  any  person 
Dow  living;  for  he  was  once  in  a  ship  which  attempted 


r^ 


*  The  Weighgatt  ie  so  called  from  the  wind  which  blows  through 
this  Strait,  {wethen,  to  blow)  because  a  strong  Southwest  wind 
Another  name  for  it  is  Hindelopen^-See  Martens's 

w 


blows  out  of  it 
Voyage,  p.  37 


.W^ 


4.- 


■m 


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%  ^' 


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THE  NORTH  POLE. 


4  ^' 


55 


f-*' 


to  pass  through  it,  nor  did  the  Master  desist,  till  they 
shoaled  the  water  to  three  fathoms,  when  the  sea 
was  so  clear,  that  they  could  distinguish  the  bottom 
from  the  deck. 

Mr.  John  Phillips,  now  Master  of  the  Exeter,  but 
then  Mate  of  the  Loyal  Club,  in  the  year  1752, 
reached  North  latitude  81'  and  several  minutes  by 
observation,  which  circumstance  was  confirmed  by 
another  person  on  board  the  Exeter  last  summer,  on 
her  return  from  the  Greenland  Fishery.  Captain 
Phiiffips  added,  that  it  was  very  eommm  to  fish  in  such' 
latitudes.  -  y  ^^ 

^:  Mr.  George  Ware,  now  living  at  Erith  in  Kent, 
served  as  chief  Mate  in  the  year  1754,  on  board  the 
Sea  Nymph,  Captain  James  Wilson,  when,  at  the 
latter  end  of  June,  they  sailed,  through  floating  ice 
from  74**  to  81";  but  having  then  proceeded  beyond 
the  ice  they  pursued  the  whales  to  82**  15',  which 
latitude  was  determined  by  Mr.  Ware's  own  ob- 
servation. <..  ^■ 

As  the  sea  was  now  perfectly  cliear,  as  far  as  he 
could  distinguish  with  his  best  glasses,  both  Mr. 
Ware  and  Captain  Wilson  had  a  strong  inclination  to 
push  farther  towards  the  Pole;  but  the  common 
sailors  hearing  of  suck  their  intention,  remonstrated, 
that  if  they  should  be  able  to  proceed  so  far,  the  ship 
would  fall  into  pieces,  as  the  Pole  would  draw  all  the 
iron-work  out  of  her. 

On  this  Captain  Wilson  and  Mr.  Ware  desisted,  as 
the  crew  had  these  very  singular  apprehensions; 
especially  as  they  had  no  whales  in  sight  to  the 
Northward,  which  alone  would  justify  the  attempt  to 


;■# 


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ON  APPROACHING 


( 


k 


their  owners.*  It  need  scarcely  be  observed,  how- 
ever, that  the  notion  which  prevailed  among  the 
crew  shows,  that  the  commoh  seamen  on  board  the 
Greenland  ships  conceive,  that  the  sea  is  open  to  the 
Pole ;  they  would  otherwise  have  objected  on  account 
of  the  ice  being  supposed  to  increase.  It  should 
seem  also,  that  the  practicability  of  reaching  the 
Pole  is  a  point  which  they  often  discuss  among 
themselves. 

In  tfUs  same  year  and  month,  Mr.  John  Adams  (who 
now  is  master  of  a  flourishing  academy  at  Waltham 
Abbey,  in  Essex)  was  on  board  the  Unicorn,  Captain 
Guy,  when  they  anchored  in  Magdalena  Bay,t  on 
the  Western  coast  of  Spitzbergen  and  North  latitude 
79"  35'.  "l 

They  continued  in  this  Bay  for  three  or  four  days,  ^ 
and  then  stood  to  the  Southward,  when  the  wind? 
freshening  from  that  quarter,  but  the  weather  foggy, 
they  proceeded  with  an  easy  sail  for  four  days, 
expecting  to  meet  with  fields  of  ice,  to  which  they 
might  make  fast ;  but  they  did  not  encounter  so  much' 
as  a  piece  that  floated.  On  the  fifth  day  the  wind 
veered  to  the  Westward,  the  weather  cleared  up,  and 
Mr«  Adams  had  a  good  observation  (the  sun  above 
the  Pole)|  by  which  he  found  himself  three  degrees 

*  This  circumstance  of  not  seeing  any  whales  in  that  direction 
accounts  for  Captain  Guy's  desisting,  in  the  following  instance,  from 
sailing  to  the  Northward,  as  also  in  many  others  which  I  shall  have 
occasion  to  state. 

t  The  Greenland  Masters  most  commonly  call  this  Bay  Mac- 
Helena.  ' 

X  Theold  navigators  to  these  parts  call  this  a  South  Sun.       ;  '    ^ 


f 


to  the  N< 
latitude  I 

Gaptai 
been  so  I 
up  to  th 
chief  mat 
Adams,  i 
they  saw 
Atlantic 
all,  that 

The  si 
hours  aft 
servatior 
tude  wa 
Adams  i 
which,  h 
on  his  fi 
Seas. 

In  the 
merchan 
then  Ma 
during  tl 
tude  83° 
ter  infori 
much  to 
the  Nort 

In  176 

was  driv 

t  minutes, 

was  bes< 

told  me 


■«•■ 


iif.. 


■•  M. 


,i 


n 


>■> 


TH£  NORTH  POLE. 


% 


57 


u- 


to  the  Nortliward  of  Hakluyf  s  Headland,  or  in  North 
latitude  83°. 

Captain  Guj  now  declared,  that  he  had  never 
been  so  far  to  the  Northward  before,  and  crawled 
up  to  the  maintopmast  head,  accompanied  by  the 
chief  mate,  whilst  the  second  mate,  together  with  Mr. 
Adams,  went  to  the  foretopmast  head,  from  whence 
they  saw  a  sea  as  free  from  ice  as  any  part  of  the 
Atlantic  Ocean,  and  it  was  the  joint  opinion  of  them 
all,  that  they  might  have  reached  the  North  Pole. 

The  ship  then  stood  to  the  Southward,  and  twelve 
hours  afterward  Mr.  Adams  had  a  second  good  ob- 
servation (the  sun  beneath  the  Pole)  when  their  lati- 
tude was  82**  3'.  In  both  these  observations,  Mr. 
Adams  made  an  allowance  of  5'  for  the  refraction, 
which,  he  says,  was  his  captain^s  rule,  who  was  now 
on  his  fifty-ninth  or  sixtieth  voyage  to  the  Greenland 
Seas. 

In  the  year  1756,  Mr.  James  Montgomery,  now  a 
merchant  in  Prescot-Street,  Goodman^s  Fields,  but 
then  Master  of  the  Providence,  followed  the  whales 
during  the  month  of  June,  till  he  reached  North  lati- 
tude 83°,  by  observation.  Another  Greenland  Mas- 
ter informs  me,  that  he  remembers  well  the  ice  packed 
much  to  the  Westward,  but  that  the  sea  was  open  to 
the  Northward  during  that  summer. 

In  1762,  David  Boyd,  then  mate  of  the  brig  Beftsy, 

was  driven  by  a  gale  of  wind  from  79°  to  82°,  odd 

I  minutes,  by  observation ;  during  all  which  time  he 

was  beset  in  ice.    A  Greenland  Master  has  likewise 

told  me,  that  he  recollects  many  other  ships  were 


m 


^■%    ^ 


K^, 


*:■:•' 


^^  •.•«»» 


A 


='«fcPsige'^ 


ii 


-m 


58 


Olf  APPROACHING 


m 


%: 


'n- 


driven  to  th«  Northeast  from  their  fishing  stations 
during  that  season. 

Mr.  Jonathan  Wheatley,  now  Master  of  a  Green- 
land ship,  was  in  1766  off  Hakluyt^s  Headland,^ 
whence,  not  meeting  with  success,  he  sailed  North- 
west to  81i%  in  which  latitude  he  could  see  no  ice  in 
any  direction  whatsoever  from  the  mast  head,  though 
there  was  a  very  heavy  sea  from  the  Northeast. 

Mr.  Wheatley  also  informs  me,  that  whilst  he  was 
off  the  coast  of  Greenland,  three  Dutch  Captains  told 
him,  that  a  ship  of  their  nation  had  been  in  89",  and 
they  all  supposed,  that  the  sea  in  such  a  latitude 
might  be  as  free  from  ice  as  where  they  were  fishing. 
This  account  probably  alludes  to  the  Dutch  man  of 
war,  on  board  of  which  Dr.  Dallie  happened  to  be, 
the  circumstances  of  which  voyage  I  have  stated  in 
my  former  Paper. 

This  same  Captain  is  so  thoroughly  persuaded  of 
being  able  to  approach  the  Pole,  that  he  will  attempt 
it  whenever  an  opportunity  offers  of  doing  it,  without 
prejudice  to  his  owners.  On  such  a  voyage  of  dis- 
covery, he  would  not  wish  a  lai^r  vessel  than  one 
of  ninety  ton8,t  nor  more  than  ten  hands.  I  find, 
indeed,  that  this  is  the  size  of  the  ships  in  which 
most  of  the  early  navigators  attempted  to  proceed  far 
to  the  Northward.  ■•  ,   • 

*  He  was  Aeii  on  board  a  ship  called  the  Grampas. 

t  Clipperton  reached  China  in  a  bait  not  much  exceeding  ten 
tons,  as  did  ako  Funnell,  in  another  such  vessel. — Cadlander,  vol. 
iii.  p.  223. 


m 


^•*.' 


'^ 


.^     ,-11     *^ 


TUf:  NORTH  POLS. 


itationfi 

Green- 
dland/ 

North- 
ice  in 

though 
It. 

le  was 
lins  told 
\9f*,  and 
latitude 

fishing. 

man  of 
I  to  be, 
tated  in 

laded  of 
attempt 
without 
(  of  dis- 
lian  one 
I  find, 
1  which 
ceed  far 


iecling  ten 
inder,  vol, 


In  1769,  Mr.  John  Thew,  now  Master  of  a  Green-  % 
land  Ship  called  tWHising  Sun,  was  in  North  lati- 
tude 82%  and  one  hundred  leagues  to  the  West  of 
Hakluyt's  Headland.  The  circumstances  by  which 
he  supposed  himself  to  have  been  in  this  situation, 
were  stated  to  me  in  the  presence  of  a  very  able  sea 
officer,  who  told  me  afterward  that  he  was  perfectly 
satisfied  with  the  accuracy  of  his  account. 

Captain  John  Clarke,  of  the  Sea  Horse,  at  the 
latter  end  of  June,  1773,  sailed  from  the  Headland 
North  Northeast  to  8U%  which  he  computed  by  his 
run  from  the  Headland  in  eighteen  hours,  having  lost 
tight  of  it.  At  this  time  there  was  an  open  sea  to  the 
Northward,  and  such  a  swell  from  the  Northeast, 
that  the  ship  would  not  stay,  being  under  her  double 
reefed  topsails,  whilst  the  wind  blew  fresh. 

During  this  run  from  the  Headland,  Mr.  Clarke  fell 
in  with  Captain  Robinson  in  81**  20',  whom  I  men- 
tioned in  my  former  Paper  as  having  reached  81i 
in  the  same  month  and  year,  by  a  very  accurate 
observation. 

This  same  Captain  Robinson,  on  the  26th  of  June 
last,  passed  by  Hakluyt's  Headland,  lying  off  and  on 
for  several  days,  during  which  he  was  sometimes  a 
degree  to  the  Northward  of  it,  and  till  the  20th  of 
July  following,  there  was  no  obstruction  to  his  pro- 
ceeding Northward ;  to  which,  however,  he  had  no 
inducement,  as  he  caught  two  large  whales  in  this 
latitude.* 

*  The  Second  Part  of  Martens'a  Voyage  (who  received  certain 
queries  from  the  Roysd  Society)  begins  almost  by  saying,  "We 
sailed  to  the  81st  degree,  and  no  ship  ventured  fartiier  that  year/' 
viz.  1671.        ;i| 


0 


*Mt. 


•«t. 


^H- 


# 


%^ 


« 


60 


ON  APPROACHING 


i*' 


Captain  John  Reed,  of  the  RocKin^hamf  also  in 
July  last,  pursued  some  whald^fiileen  leagues  to  the 
Northward  of  the  Headland,  and  confirms  Captain 
Robinson^s  last  account,  by  saying,  he  could  then  see 
no  ice  from  his  mast  head. 

Captain  Reed  was  brought  up  in  the  Greenland 
fishery,  and  remembers  well,  that  whilst  on  board  his 
father's  ship,  the  Thistle,  the  mate  told  him,  that 
they  had  reached  81"  42',  when  there  was  indeed  a 
good  deal  of  ice,  but  full  room  to  sail  in  any  direction. 
Mr.  Reed  likewise  hath  informed  me,  that  about 
fifteen  years  ago,  a  Dutch  Captain  (whose  name  was 
Hans  Derrick)  told  him,  whilst  they  were  together  in 
the  Greenland  Seas,  that  he  had  been  in  North  lati- 
tude 86**  when  there  were  only  some  small  pieces  of 
floating  ice  to  be  seen.    Hans  Derrick  moreover 
added,  that  there  were  then  five  ships  in  company, 
which  took,  one  with  another,  eighteen  small  whales. 
I  have  great  reason  to  expect  several  other  instan- 
ces of  the  same  kind,  in  a  short  time,  fi>om  the  dif- 
ferent ports  of  this  kingdom  where  there  is  any  con- 
siderable Greenland  trade:  I  shall  not,  however, 
trouble  the  Sojciety  with  them,  till  I  know  whether 
they  would  wi^h  any  farther  information  on  this  head. 
I  shall    now  recapitulate  the  different  latitudes 
which  have  been  reached  by  the  several  navigators 
whose    names  I  have  mentioned   in  this  and  my 
former  Paper.    I  shall  also  take  credit  for  nearly  a 
degree  to  the  Northward  of  their  several  situations, 
because  the  blink  or  glare  of  the  packed  ice  is  to  be 
distingpished  at  this  distance,  when  the  weather  is^ 
tolerably  feir. 


Capta 
Capta 

t 
Capta 
Jamet 

I 
Capta 
Clunj 
Mr.  C 
Mr. 

Mr. 

Five 

Capts 


Relat 
Dutcj 

*  This 
nerer,  pe 


f'ftf&V 


»    ' 


HI* 


THE  NORTH  POtl.  "  61 

Captain  John  Reed 80*  46^. 

Captain  Thonuu  Robinson  (for  three  weeks 

together) 81®. 

Captain  John  Phillips 81    odd  mi. 

James  Button,  Jonathan  Wheatley,  Thomas 

Robinson,  John  Clarke  (four  instances)  81*  SO. 

Captain  Cheyne  and  Thew  (two  instances)  .  82°. 

Cluny  and  David  Boyd  (two  instances)    .  .      82*  odd  mi. 

,   Mr.  George  Wpxe 82°  16' 

'      Mr.  John  Adams  and  Mr.  James  Montgomery 

(two  instances) 83°. 

Mr.  James  Watt,  Lieutenant  in  the  Royal 

Navy - 83°  30'. 

Five  ships  in  company  with  Hans  Derrick  .  .  86°* 

Captain  Johnson  and  Dr.  Dallie  (two  instan- 
ces; to  which,  perhaps,  may  be  added 
Captain  Monson,  as  a  third) 88°. 

Relation  of  the  two  Dutch  Masters  to  Captain 

Goulden* 89°. 

Dutch  relation  to  Mr.  Grey 89°  3Cf. 

n^IJ^ES  BARBIJ^GTOJiT,  F.R.S. 

*  This  instance,  however,  hath  before  been  relied  upon,  though 
aever,  perhaps,  circumstantially  stated,  but  by  Captain  Wood. 


M  ;■< 


:A 


■\ 


•     4 


'■* 


•      «%     .     -.1 


,     ,1    >•   , 


,j 


#' 


A' 


V  .■*,. 


H 


S*^ 


POSTSCRIPT. 


■^  ■■&.■ 


:  :,  u      -H. 


»w4^' 


ife;. 


January  8,  1775. 

Having  procured  the  three  following  instanceB 
before  the  reading  of  my  Paper  was  finiehed,  it  may 
not  be  improper  to  add  them  in  a  PoBtscript. 

f n  Harrises  Voyages*  is  the  following  passage  :— 
**  By  the  Dutch  Journals  they  get  into  North  latitude 
8{f  56',  and  the  sea  open/* 

I  have,  within  these  few  days,  asked  Dr.  Campbell, 
the  very  able  compiler  of  these  voyages,  upon  what 
authority  he  inserted  this  account  ?  who  informs  me, 
that  he  received  it  from  Holland  about  thirty  years 
ago,  as  being  an  extract  from  the  Journals  produced 
to  the  States  General  in  1665,  on  tlie  application  for 
a  discovery  of  the  Northeast  passage  to  Japan,  which 
was  frustrated  by  the  Dutch  East-India  Company. 

In  the  Journal  des  Sgavans,  for  the  month  of  October 
1774,t  is  likeidse  the  following  paragraph : — 

»'  To  these  instances,  produced  by  Mr.  Barrington** 
(of  navigators  having  reached  high  Northern  lati- 
tudes,) **  our  countrymen"  (viz.  the  Dutch)  "  could 
add  many  others.  An  able  officer  in  the  English 
service  hath  in  his  custody  the  Journals  of  a  Green- 
land ship,  wherein  he  hath  remarked,  that  in  the 
month  of  May  he  had  penetrated  as  far  as  82**  20', 
when  the  sea  was 


Vol. 


open. 


ii.  page  453. 


t  Part  ii.  page  503. 


\ 


r 

4 


...«. 


I 


^*- 


;,^^     ■iS'l 


'/-3^'* 


64 


ON  APPROACHING 


m 


t 


i 


ST. 


My  third  and  last  instance  is  that  of  Captain 
Bateson,  who  sailed  in  1773  from  Liverpool,  in  a 
ship  called  the  Whale,  on  the  Greenland  Fishery, 
and  who,  on  June  14,  reached  North  latitude  82°  15', 
computed  by  his  run  back  to  Hakluyt's  Headland* 
As  this  happened  so  recently,  Captain  Bateson  (as 
well  as  many  of  the  other  Masters,  whose  accounts  I 
h^ve  before  mentioned)  hath  his  Journal  to  produce, 
if  it  should  be  required. 

This  seems  to  be  the  strongest  confirmation  of  both 
Captain  Robinson  and  Captain  darkens  having  been, 
during  this  same  year  and  month,  in  8li°;  as  also  of 
their  having  met  each  other  in  81**  20',  according  to 
what  I  have  already  stated. 

I  must  not  lose  this  same  opportunity  of  laying 
before  the  Society  the  information  which  I  have  just 
now  received  from  M.  de  Bufibn,  in  relation  to  what 
I  have  cited  from  his  Natural  History  of  Captain 
Monson^s  having  reached  North  latitude  88%  ^^  cts  he 
was  told  b^  persons  of  credit,''^  *;    , 

Upon  my  taking  the  liberty  to  inquire,  who  those 
persons  of  credit  were  ?  M.  de  Bufibn  refers  me  to  Dr. 
Nathan  Hickman,  who,  in  1730,  travelled  as  one  of 
Dr.  RatclifTs  fellows  ;t  and  who  supposed  that  Cap- 
tain Monson'fl  Journal  might  have  been  at  that  time 
procured  in  England.  M.  de  Buiibn  also  recollects, 
that  a  Dutchman  was  then  present,  and  confirmed 
the  account. 

*  His  inducement  to  proceed  so  far  North  was  the  pursuit  of  whales. 
I  hare  shown  the  extracts  from  Captain  Bateson's  Journal  to  a  very 
able  sea  officer,  who  is  perfectly  satisfied  with  the  accuracy  of  it. 

t  He  was  also  a  Fellow  of  the  Royal  Society  in  1730. 


Whil 

addition 
in  high 
answers 
Seas  fr 
which  1: 
the  pub 


i?j« 


March 


Hi; 


•v 


FiK 
theP< 

AnE 
of  84" 


HF 


#«. 


..     ■^■ 


# 


^*'i 


'■*.'.. 


[ptaih 
in  a 
[herj, 

land* 
(as 
ints  I 
luce, 


f 


^     " 


THE  NORTH  P0IJ2. 


6S 


ADDITIONAL  PAPEB8 


■i-.»- 


.,^s 


WtLOU 


*t. 


HULL. 


»9« 


M,A^^.  .-v 


A^HILST  I  was  waiting  in  expectation  of  several 
additional  instances  of  Dutch  ships,  which  had  been 
in  high  Northern  latitudes,  I  received  the  following 
answers  to  certain  Queries  relative  to  the  Greenland 
Seas  from  a  very  eminent  Merchant  of  Hull,  and 
which  he  is  so  obliging  as  to  permit  me  to  lay  before 
the  public. 


D.  B- 


March  31,  1775. 


fi>...y,:-''    . 


»«« 


l$i 


I 


FROM  CAPTAIN  JOHN  HALL, 


OF 


*5^  '*■■■ ,«' 


THE  KING  OF  PRUSSIA. 


First  Query.  How  near  hath  any  ship  approached 
the  Pole? 

Answer.  I  have  known  ships  go  into  the  latitude 
of  84**  North,  and  did  not  hear  of  any  difficulty  they 

9 


W""    ■^ 


,)«^ 


■t* 


:%■ 


^ 


'^•■ 


*#^" 


66 


ON  APPROACHING 


t' 


met  with ;  but  it  is  not  often  that  the  ice  will  permit 

them  to  go  so  far  North. 

N.  B.  On  inquiring  of  Captain  Hall  what  ships  he 
had  known  proceed  bo  far?  He  replied,  they 
were  some  Dutch  ships  he  heard  ha^  done  so, 
but  knew  no  particulars.  • 

Second  Q.  When  are  the  Polar  Seas  most  free 
from  ice  ? 

A.  The  seas  are  most  incumbered  with  ice  from 
about  thejst  of  September  to  the  1st  of  June  follow- 
ing; and,  in  consequence,  between  the  1st  of  June 
and  September,  the  ice  lieth  farthest  from  Spitz- 
bergen.  And  I  know  no  other  precaution  to  be  taken, 
respecting  the  Pole,  than  that  they  must  watch  the 
opportunity  when  the  ice  lieth  farthest  from  the  land. 

Thiid  Q.  How  far  to  the  Southward  have  you 
first  sken  ice?  ,  .         » 

A.  In  the  space  of  twenty  years  I  have  twice 
known  that  we  met  with  the  ice  in  the  latitude  of 
74"  30'  North,  and  could  not  find  a  passage  to  the 
Northward  till  the  month  of  July,  and  then  got  into 
the  latitude  of  78**  with  much  difficulty,  in  running 
through  the  openings  of  great  bodies  of  ice;  and 
some  years  we  find  a  passage  to  the  latitude  79  and 
80°  North,  without  much  difficulty  from  the  ice.  Some 
years  I  have  known  ships  go  round  the  North  part  of 
Spitzbergeny.  and  so  come  out  between  Nova  Zembla 
and  the  South  part  of  Spitzbergen ;  but  this  passage 
is  seldom  to  be  found  free  from  ice. 


Fourth 
whilst  oflf 
A.  N< 
frosty;  b 
with  all 
August, 
milder,  b 
The  win 

The 

proceed 

attemptc 

opportui 

most  lik 

the  mon 

commor 

to  be  fo 

is  open, 

from  tl 

known 

ward,  i 

with  tl 

leave  i 

N.B. 

oftl 


k 


■:4^  -^l 


Fir 
Nortl 


,■  # 


'*f 


».*  „     .  -ij, 


•yf  V  '^«#JH«>'»>.>^~ 


permit 


st  free 


H 


THE  NORTH  POLE. 


67 


MtJi^^ui. 


Fourth  Q.  From  what  quarter  is  the  wind  coldest 
whilst  off  Spitzbergen? 

A.  Northerly  and  East  Northeast  winds  are  most 
frosty;  but  snow  and  frost  we  have  very  common 
with  all  winds,  except  during  part  of  June,  July,  and 
August.  If  the  winds  be  Southerly  the  weather  is 
milder,  but  subject  to  snow-  sleet,  and  thick  weather. 
The  winds,  currents,  and  the  ice,  are  very  variable. 

The  opinion  of  the  old  seamen  is,  that  we  may 
proceed  farther  North  than  ever  has  been  yet 
attempted ;  but  this  must  be  done  with  caution.  An 
opportunity  is  to  be  watched  for  in  those  seas.  The 
most  likely  time  for  such  discoveries  to  be  made  is  in 
the  months  of  July  and  August,  when  the  ice  is  most 
commonly  farthest  from  the  land ;  but  some  years  not 
to  be  found  open  at  all  from  the  land.  And  when  it 
is  open,  they  must  observe  the  ice  to  lay  a  long  way 
from  the  North  part  of  Spitzbergen;  for  I  have 
known  ships  that  made  attempts  to  go  to  the  North-* 
ward,  and  before  they  returned  back  the  ice  set  in 
with  the  land,  so  that  they  have  been  obliged  to 
leave  the  ships  to  the  East  of  Spitzbergen. 
N.  B.    The  ice  always  sets  in  with  the  land  the  back 

of  the  year. 


-f'ii 


,•  .  '.Jf-jt. 


II. 


vH  ^ 


,.u    FROM  CAPTAIN  HUMPHRY  FORD, 


or 


THE  MANCHESTER. 


First.    I  was  once  as  high  as  the  latitude  81*  30' 
North,  in  the  ship  Dolphin  of  Newcastle,  in  the  year 


K 


■  x 


.\.     .  ^-^., 


..•'.■«i'^ 


1* 


f       o 


f 


^•., 


♦* 


4W 


"i- 


ON  APkROACHlNO 


1759  or  66,  and  have  been  several  times  since  as  high 
as  the  latitude  81°  in  the  ships  Annabella  and  Man- 
chester, in  which  latitude  I  never  met  with  any  un- 
common circumstances,  but  such  as  I  have  met  with 
in  the  latitudes  75,  76,  77,  78,  and  79"  j  if  to  the 
Westward,  I  was  commonlj  incumbered  with  large 
quantities  of  ice. 

Second.  I  suppose  that  the  Greenland  Seas  are 
most  i  '^cumbered  with  ice  in  the  months  of  Decem- 
ber, January,  February,  ana  March ;  for  in  the  latter 
part  of  April,  and  the  first  of  May,  the  ice  generally 
begins  to  separate  and  open ;  and  in  the  months  of 
June  and  July  we  generally  find  the  Greenland  Seas 
most  clear  of  ice. 

Third.  The  only  precaution  to  be  taken,  in  order 
to  proceed  towards  the  Pole,  is  to  fit  out  two  strong 
ships  that  are  handy  and  sail  fast,  well  equipped,  and 
secured  in  the  manner  of  those  that  are  generally  ^ 
sent  to  Greenland  on  the  Whale  Fishery.  Such 
ships  should  be  manned  with  about  forty  able  seamen 
in  each,  and  victualled  for  about  eighteen  months  or 
two  years,  and  be  entirely  under  the  command  of 
some  expert,  able,  and  experienced  seaman,  who  has 
fi'equented  those  seas  for  some  time  past  They 
should  sail  from  England  about  the  middle  of  April, 
in  order  to  be  in  with  the  edge  of  the  ice  about  the 
10th  of  May,  when  it  begins  to  separate  and  open. 

Fourth.  There  is  not  the  least  reason  to  suppose, 
that  the  seas  to  the  West,  Northwest,  and  North  of 


Sk 


Spitzberg 

petual  ic< 

of  the  wi 

Northerly 

and  sepa 

amongst 

attempte 

N.B. 

but  ai 

there 

%bergei 

i  gen 

and  sno 

mild  w« 

appear 

land,  cj 

the  win 

mostly  1 

give  str< 

It  is 

some  y 

not,  th 

quantit 


1  an 
theQ 

tions  ^ 


%     .  '^^^ 


-Wli. 


tu 


'««* 


[as  high 
Man- 
iny  un- 
it with 
to  the 
large 


kf^ 


'  1 


■4 


5'- 


# 


THE  NORTH  POLE. 


69 


Spitzbergen  are  covered  with  permanent  and  per- 
petual  ice,  so  as  never  to  be  opened  by  the  operation 
of  the  windis;  for  daily  experience  shows  us,  that  a 
Northerly  wind,  when  of  any  long  duration,  opens 
and  sepTurates  the  ice,  so  as  to  admit  the  ships  going 
amongst  it  in  sundry  places  to  a  very  high  latitude,  if 
attempted. 

N.  B.  I  never  was  to  the  Eastward  of  Spitzbergen; 
but  am  of  opinion,  that  the  ice  is  much  the  same 
there  as  to  the  North  and  Northwesf  of  Spitz- 
bergen. 

,1  generally  find,  that  Northerly  winds  bring  frost 
and  snow ;  on  the  contrary,  Southerly  winds  bring 
mild  weather  and  rain;  but  none  of  those  winds 
appear  to  be  periodical,  except  close  in  with  the 
land,  called  Fair  Foreland,  where  1  generally  find 
the  winds  in  the  months  of  June  and  July  to  blow 
mostly  from  South  Southwest,  and  very  often  exces- 
sive strong. 

It  is  my  opinion,  by  observing  the  above,  that  in 
some  years  ships  might  sail  very  nigh  the  Pole;  if 
not,  the  impracticability  must  arise  from  the  large 
(quantity  of  ice  that  lies  in  those  seas. 


in. 

FROM  CAPTAIN  RALPH  DALE, 

THE  ANN  AND  ELIZABETH. 

I  am  willing  to  give  you  my  opinion,  in  regard  to 
the  Queries  received  of  you,  so  far  as  my  observa- 
tions will  justify.  ^   V 'pi 

*         .  "Tit 

.      ! 


V*-"       I 


i,t. 


V 

m 


I 


*; 


f 


■^ 


¥? 


ON  APPROACHINO 


,i 


First.  In  the  year  1773,  I  sailed  North  81%  when 
I  was  much  incommoded  with  large  fields  of  ice,  but 
the  air  was  not  sensibly  different  there  firom  what  I 
found  it  a  few  more  degrees  Southerly. 

Second.  I  have  for  many  years  used  the  Green- 
land Fishery ;  and  have,  by  experience,  found  those 
seas  the  least  incumbered  with  ice  betwixt  the  fore- 
part of  May  till  July. 

Third.  The  same  year  I  sailed  to  the  latitude 
above  mentioned,  I  found  in  May,  to  the  West  of 
Spitzbergen,  a  fine  open  sea,  the  wind  then  blowing 
Southwest,  and  the  sea  (as  far  as  I  could  observe 

A 

fi'om  the  mast-head)  was  little  incumbered  with  ice,' 
which  fully  convinced  me  that  there  was  a  probability 
of  proceeding  to  a  very  high  latitude. 

Fourth.  I  have  observed,  that  let  the  wind  blow 
from  what  quarter  it  will,  it  is  at  times  impregnated 
with  frost,  snow,  Sic. ;  but  when  most  so  I  am  not 
able  to  determine.  As  for  rain,  I  do  not  recollect 
ever  seeing  any  there.  The  weather  I  have  generally 
found  mildest  when  the  wind  blows  Southerly.  As 
for  periodical  winds,  I  do  not  suppose  there  are  any 
in  Greenland. 


FRO 

In  rega 

say  is,  it 

be  accoi 

by  going 

myself  hi 

reached 

tude,  an 

nothing 

fore,  is, 

that  waj 

Compan 

tude,  ar 

with  not 

to  the  TV 

the  win 

rain  ant 

latter  ei 

ward  ai 

Northw 

the  ice 

any  tia 

land;  i 

central 


\-. 


rUil:-.^  VI"'  m'K 


about  ni 


"*■' 


1-  /■ 


THE  NORTH  POLE: 


71 


when 
ce,  but 
what  I 


Green- 
those 
le  fore- 


atitude 
ieat  of 
•lowing 
'bserve 
ith  ice,' 
>abilitj 


I  blow 
gnated 
wn  not 
collect 
lerally 
7'  As 
re  any 


,n 


IV. 


FROM  CAPTAIN  JOHN  GREENSHAW. 

In  regard  to  the  Queries  sent  to  me,  all  I  have  to 
say  is,  that  if  a  passage  to  the  North  Pole  is  ever  to 
be  accomplished,  my  opinion  is,  it  must  be  obtained 
by  going  betwixt  Greenland  and  Nova  ZembIa,  as  I 
myself  have  been  to  the  Westward  of  Greenland,  and 
reached  bo  far  to  the  Northward  as  82°  of  North  lati- 
tude, and  to  the  North  and  Northwest  of  that,  found 
nothing  but  a  solid  body  of  ice :  my  opinion,  there- 
fore, is,  that  it  is  impossible  ever  to  obtain  a  passage 
that  way.  Captain  Jolm  Cracroft,  in  the  South  Sea 
Company's  time,*  was  once  so  far  as  83"  North  lati- 
tude, and  to  the  Northward  of  Greenland,  and  met 
with  nothing  but  a  solid  field  of  ice.  And  in  regard 
to  the  winds  and  weather,  it  freezes  continually ;  but 
the  wind  from  the  Southward  doth  commonly  bring 
rain  and  thick  foggy  weather,  which  is  chiefly  in  the 
latter  end  of  June  and  July.  If  you  are  to  the  North- 
ward and  Westward  of  Greenland  the  wind  from  the 
Northwest  and  North  Northwest,  doth  always  open 
the  ice ;  but  at  the  same  time,  if  it  come  to  blow 
any  time  from  that  quarter,  packs  it  close  in  with  the 
land ;  and  the  winds  from  the  Southward  have  the 
contrary  effect. 


M^( 


%> 


-^' 


J} 

i 


r 


J^-Va- 


The  South  Sea  Company  sent  a  small  number  of  ships,  for 


about  nine 


years, 


on  the  Greenland  Fisbcrv. 


.^...,\^..,^, 


^'^ 


:|iL 


m 


'i^t'* 


-""**-*"  j"**-*^ 


.^'' 


•lr% 


n 


ON  APFROACHINU 


V 


m 


V. 
THE  QUERIES  ANSWERED 

■T  - 

ANDREW  FISHER, 

,  MASTER  OF  A  GREENLAND  SHIP  AT  HULL, 
Who  hat  been  twetUy-four  voyages  from  England  to  the  GreenUmd  Seat. 

First.  Said  Andrew  Fisher  says,  that  in  the  year 
1746,  being  on  board  the  ship  Ann  and  Elizabeth 
from  London,  on  a  voyage  to  the  Greenland  Seas,  he 
steered  from  Hakluyt's  Headland  in  Spitzbei^en 
North  and  Northwest  in  clear  water  till  they  were  in 
latitude  82**  ^4',  where  they  met  with  a  loose  pack  of 
ice,  and  made  their  fishery,  or  otherwise  they  might 
have  got  through  that  loose  ice,  and  doubt  not,  but 
thati  they  might  have  gone  considerably  farther 
North;  they  returned,  however,  in  clear  water  to 
Spitzbergen. 

.  Second.  Best  seasons  of  the  year  are,  to  be  at  or 
near  Spitzbergen  from  the  15th  of  May  to  the  1st  of 
June,  though  the  years  difier,  and  the  laying  of  the 
ice  exceedingly :  some  years  it  is  not  possible  to  get 
North  of  80** ;  at  other  times  you  may  meet  with  very 
little  ice,  which  is  chiefly  owing  to  the  weather  in 
winter,  and  the  winds  in  April  and  May. 

Third.  There  is  not  any  reason  to  suppose,  that 
there  is  any  permanent  ice,  either  North  or  West  of 
Spitzbergen,  so  far  as  90**;  and  it  hath  b«en  always 


#. 


m 


found,<^j 
there  is  no 
set  fast  t( 
the  South 
of  Ameri< 
apd  Spitz 
proportioi 
The  lan^ 
Greenlan( 
it  is  not  s( 
away  to  t] 
many,  thi 

Fourth 
winds  br 
and  two-t 
10th  of  J< 
weather, 
thick  fog 

Fifth. 
North  N 
so  contri 
and  the 
verance, 
meet  wi 


iH'. 


V       .      SIR, 


ship  at 


■-;.    ,,.^' ■■<'*;• 


1*  ir- 


THE  NORTH  POLE. 


73 


iland  Seat. 

the  year 

llizabeth 

Seas,  he 

zbergen 

were  in 

pack  of 

ej  might 

not,  but 

'  farther 

/rater  to 


be  at  or 
le  1st  of 
^  of  the 
le  to  get 
ith  very 
ither  in 


se,  that 

iVest  of 

always 


S    r.* 


found,  ^y  able  and  experienced  navigators,  that 
there  is  not  near  the  quantity  of  ice,  nor  so  liable  to 
set  fast  to  the  North  of  Spitzbergen,  as  there  is  to 
the  South  of  80°  as  far  as  74%  owing  to  the  continent 
of  America  (called  Gallampus  Land  by  the  sailors) 
and  Spitzbergen,  which  makes  a  narrow  passage  in 
proportion  to  what  it  is  to  the  North  of  Spitzbergen. 
The  land  of  America  is  sometimes  seen  by  our 
Greenland  Traders  from  latitude  74"  to  76";  and,  as 
it  is  not  seen  any  farther  North,  is  supposed  to  round 
away  to  the  Northwest,  which  makes  it  imagined  by 
many,  that  there  is  not  any  land  near  the  Pole. 

Fourth.  South  winds  bring  most  snow;  North 
winds  bring  frost ;  but  that  is  in  the  month  of  April 
and  two-thirds  of  May;  after  that  time,  to  the  1st  or 
10th  of  July,  it  is  in  general  mild,  fine,  clear,  sunshine 
weather,  and  winds  variable ;  after  that  again,  often 
thick  fogs  and  high  winds. 


ni 


Fifth.  It  is  very  possible,  by  steering  North  or 
North  Northeast  by  the  ship^s  compass,  (if  it  can  be 
so  contrived  as  to  have  the  card  on  the  needle  steady, 
and  the  winds  prove  favourable,)  with  a  little  perse- 
verance, a  ship  may  get  near  the  Pole,  if  they  do  not 
meet  with  rocks. 


VI. 


.i   '.1>^«|,. 


SIR, 


In  the  year  1766,  trade  being  dull,  I  fitted  a 
ship  at  my  sole  expense  to  the  Greenland  ,_eas ;  and 

10 


n 


1 1 


:V- 


i 


%-. 


-.*,j,jiM'*(-   *«-"*■  ••*«3l^  4 


-A^^..rr 


•^. 


74 


ON  APniOACHIir« 


tiie  said  ship  returned  with  one  fish,  eleven  feet  bone. 
Finding  the  trade  could  be  conducted  better  in  pri- 
vate hands  than  a  company^s,  I  was  induced  to  send 
a  second  ship  in  1767,  and  as  I  had  other  concerns 
in  shipping,  thought  it  most  prudent  (being  brought 
up  to  the  sea,  and  having  made  an  easy  fortune  from 
it)  to  go  a  voyage  to  the  Greenland  Seas,  to  see  with 
my  own  eyes  what  chance  there  might  be  of  making 
or  losing  a  fortune.  So  sailed  from  Hull  the  14th 
^ay  of  April,  in  my  ship  British  Queen,  with  an  old 
{Experienced  Master,  and  on  the  24th  and  25th  of 
April  was  in  the  latitude  of  72%  catching  seals  amongst 
great  quantities  of  loose  ice.  As  we  did  not  choose 
to  stay  in  that  latitude,  we  made  the  best  of  our  way 
North ;  and  after  sailing  through  loose  ice,  which  is 
commonly  the  case,  about  the  6th  of  May  we  were 
as  far  North  as  latitude  80**  (which  is  near  what  the 
Masters  call  a  fishing  latitude)  and  about  fifteen  leagues 
West  of  Hakluyt^s  Headland.  I  found  the  farther 
North  the  less  quantity  of  ice ;  and  from  the  inquiry 
I  made,  both  from  the  English  and  Dutch,  which  was 
very  considerable,  there  is  a  great  probability  of 
shipi^  going  to  the  Pole,  if  not  stopped  by  meeting 
land  or  rocks.  It  appeared  to  me,  that  the  narrowest 
place  in  those  seas  was  betwixt  Spitzbergen  and  the 
American  shore,  where  the  current  is  observed  to 
come  always  from  the  North,  which  fills  this  narrow 
place  with  ice,  but  in  general  loose  and  floating  in 
(he  summer,  though  I  believe  congealed  and  perma- 
nent in  winter.  Thpse  from  whom  I  inquired  inform- 
ed me,  that  the  sea  was  abundantly  clearer  to  the 
North  of  Spitzbergen,  and  the  farther  North,  the 


.^ 


^/ 


i% 


^A*^'- 


THE  NORTH  POLE. 


75 


feet  bone. 
ler  in  pri^ 
to  send 
concerng 
brought 
:une  from 
see  with 
|f  making 
the  14th 
th  an  old 
1  25th  of 
s  amongst 
ot  choose 
four  yray 
which  is 
we  were 
what  the 
Jn  leagues 
le  farther 
>e  inquiry 
t^hich  was 
ability  of 
meeting 
arrowest 
I  and  the 
erved  to 
narrow 
>ating  in 
!  perma- 
inform- 
r  to  the 
th,  the 


clearer.  This  seems  to  prove  a  wide  ocean  and  a 
great  opening  to  the  North,  as  the  current  comes 
from  thence,  that  fills  this  passage  as  aforesaid.  The 
best  method  of  reaching  the  highest  latitude,  in  my 
opinion,  is,  to  hire  two  vessels  of  about  two  hundred 
and  fifty  tons  burthen  each,  and  if  done  on  a  frugal 
scheme,  the  same  ships  might  be  fitted  for  the  whale 
fishery,  and  premiums  given  both  for  the  use  of  the 
ship  and  crew,  in  proportion  to  their  approach  to  the 
Pole,  which,  for  many  circumstances  that  may  inters 
vene,  might  be  two  or  three  years  before  they  could 
complete  their  wishes.  And  it  is  more  likely  they 
might  make  their  fishery  sooner  than  to  the  South- 
ward ;  as,  if  they  met  with  ice,  the  fish  would  be 
undisturbed ;  if  clear  water  and  a  good  wind,  they 
very  soon  might  reach  the  Pole.  What  I  mean  by 
two  vessels  is,  one  to  foresail  the  other  at  the  dis« 
tance  of  three  or  four  leagues,  as  the  latter  may 
avoid  the  dangers  the  first  might  run  into;  and  to  be 
always  ready,  on  seeing  and  hearing  proper  signals^ 
to  aid  and  assist,  and  by  that  means  secure  a  retreat. 
I  am  also  of  opinion,  that  such  ships  being  sent  on 
discoveries  are  much  more  likely  to  succeed  than  his 
Majesty^s  ships  and  officers.  The  above  hints  I  have  • 
pointed  out  for  your  consideration ;  and,  if  I  cap  be 
of  any  farther  service,  may  command, 

Sir, 
i ,  t  Your  most  humble  Servant, 


SAM.  STANDIDGB> 


WuUy  March  4, 1774. 


.^i.;rf»- 


ir 


'«i^ 


ON  APPROACHING 


I  take  this  oppoi'tuiiity  of  laying  before  the  Public 
the  following  letter  from  Captain  Marshall,  Master  of 
ft  Greenland  shipv  to  Captain  Heath  of  the  4lBt 
Regiment,  who  formerly  made  two  voyages  to 
Spitzbergen. 


i.^ttl 


SIR, 


* 


I.;  In  compliance  with  your  request  of  Wednes- 
day last,  I  acquaint  you,  that  six  years  ago  I  was  as 
high  as  82"  30'  North  latitude,  by  observation,  which 
is  the  highest  I  have  ever  been  in ;  at  that  time  I  was 
Mate  of  the  Royal  Exchange  Greenlandman,  of  New- 
castle. I  do  not  know  of  any  one  who  has  been  in  a 
higher  degree ;  but  it  has  been  reported  at  Newcastle 
(with  what  truth  I  cannot  say)  that  Captain  Green- 
shaw,  of  London,  had  told  his  friends,  that  he  had 
been  as  high  North  as  84^ 

The  Dutch,  I  have  been  informed,  have  proceeded 
to  83**  30';  but  I  have  it  only  by  hearsay. 

In  respect  to  your  second  Query,  I  remember,  that 
about  five  years  since,  when  I  was  Master  of  the 
above-mentioned  ship,  I  was  in  81"  North  latitude, 
by  observation,  when  there  was  a  clear  sea  to  the 
Northward,  as  far  as  the  eye  could  reach  from  the  mast 
head ;  and  I  could  not  help  observing  to  my  people, 
that  if  it  had  happened  that  we  were  then  upon  dis- 
covery, we  might  have  had  a  fine  run  to  the  North, 
as  the  wind  blew  fresh  at  South.  The  like  clear  sea 
I  have  observed  several  times  during  the  time  I  have 
been  in  the  Greenland  service,  which  is  now  about 
twenty-one  years.  I  have  no  doubt  but  that  a  navi- 
gator might  reach  a  higher  latitude  than  I  have  been 


ill,  provi 
rents  an 
took  the 
remarke 
Englanc 
great  d< 
mer  tha 
bly  fine 
cxpectt 
duce  a 
an  opp< 
But 
very  hi 
should 
would 
along 
from  \ 
monthi 
gotou 


I'llE  NORTH  POLE. 


Public 
faster  oi' 
(he  41  St 
iges    to 


ednes- 
was  as 
♦  which 
>e  I  was 
ofNew- 
ien  in  a 
wcastle 
Green- 
he  had 

)ceeded 

■  *, 
er,  that 

of  the 
atitude, 

to  the 
Fie  mast 
people, 
on  dis- 
North, 
Jar  sea 
I  have 

about 
'  navi- 

been 


ill,  provided  he  was  well  acquainted  wilh  the  cur- 
rents and  the  ice,  (for  much  depends  thereon,)  and 
took  the  advantage  of  a  favourable  season.  I  havo 
remarked,  that  when  the  frost  has  been  severe  in 
England,  and  to  the  Southward,*  there  has  been  a 
great  deal  less  ice  to  the  Northward  the  ensuing  sum- 
mer than  usual ;  and  the  weather  has  been  remarka- 
bly fine  in  Greenland.  I  have,  for  this  reason,  great 
expectations  that  the  approaching  season  will  pro- 
duce a  successful  fishery,  and  that  it  will  also  afibrd 
an  opportunity  for  a  trial  to  reach  the  Pole.t  ^ 

But  the  greatest  difficulty  attending  a  navigator  in 
very  high  latitudes,  is  how  to  get  back  agaui,  for, 
should  he  be  beset  there  in  the  ice,  his  situation 
would  be  very  dangerous ;  for  he  might  be  detained  ' 
a  long  time,  if  not  for  the  whole  winter.  I  speak  this 
from  experience,  for  I  was  once  beset  for  three 
months,  and  was  given  up  for  lost,  and  with  difficulty 
got  out. 


*  I  conceive  that  this  arises  from  the  ice  becoming  of  a  greater 
thickness  during  such  severe  winters,  and  consequently  cannot  be  so 
soon  broken  up,  or  observed  by  the  Greenland  ships,  which  return 
to  the  Southward,  before  the  ice  can  have  floated  to  them  in  thf: 
Spitsbergen  Seas.  ^ 

" '.  C    \C'  '  ., 

t  I  am  sorry  to  hare  been  informed,  since  the  Bill  for  promoting 
biscoveries  passed,  that  the  attempts  to  penetrate  to  the  Northward 
will  not  be  so  frequent  as  I  had  flattered  myself;  because,  most  of 
the  Greenland  vessels  being  ensured,  if  any  accident  should  happen 
to  a  ship  which  is  not  prosecuting  the  Whale  Fishery,  the  owners 
will  not  be  entitled  to  recover. 


r 


*■»•'• 


% 


78 


ON  APPROACHING 


1^ 


I   I 


Any  farther  information  in  respect  to  the  land,  the 
currents,  ice,  or  other  particulars,  you  may  wish  to 
have,  I  shall  very  readily  communicate  it,  and  am, 
Sir, 
Your  very  humble  Servant, 

JAMES  MARSHALL.  , 

jVo.  6,  Spring-Street,  Shadwell^ 
Fxiltruary  26,  1776. 


Cap^in  Heath,  to  whom  I  am  indebted  for  this 
communication,  also  informs  me,  that  on  the  15th 
of  December,  1777,  he  minuted  the  following  particu- 
lars from  a  person  employed  in  the  whale  fishery. 


•■'■h'fX-'^s'^'f:- 


# 


"That  being  on  boai'd  the  Prince  Frederick  of 
Liverpool  in  1765,  commanded  by  James  Bisbrown, 
he  reached  the  latitude  of  83**  40*,  where  he  was 
beset  in  ice  for  three  weeks,  to  the  Southward,  but 
that  he  saw,  during  this  time,  an  open  sea  to  the 
North."         ..  .  . 


■0: 


'^mm: 


v^(»i*'  \ 


The  Astronomer  Royal  having  b^eft  so  good  as  to 
furnish  me  with  the  following  memorandum,  which  he 
made  at  the  time  it  bears  date,  I  here  subjoin  it,  as 
a  well-authenticated  instance  of  a  navigator^s  having 
reached  84^**  of  Northern  latitude. 


.■K   ^**V^  .. 


"Mr.  Stephens,  who  went  many  voyages  to  the 
East  Indies,  and  made  much  use  of  the  lunar  method 
of  finding  the  longitude,  in  which  he  is  very  expert, 


'■fir- 


:/><"'■ 


J        %> 


/ 


M 


THE  NORTH  POLE. 


79 


I 'and,  the 
wish  to 
id  am, 

[ALL. 

for  this 
the  15th 
particu- 
leiy.    - 

erick  of 
isbrown, 
he  was 
*rd,  but 
to  the 

d  as  to 
iuch  he 
I  it,  as 
having 


to  the 
lethod 
Xpert, 


telle  me,  this  16th  of  March,  1773,  that  he  was  form- 
erly two  voyages  on  the  Greenland  fishery ;  that,  in 
the  second,  in  the  year  1754,  he  was  driven  off  Spitz- 
bergen,  together  with  a  Dutch  ship,  by  a  .South 
Southeast  wind,  North  Northwesterly  by  compass  into 
latitude  844%  or  within  54"  of  the  Pole,  in  which  lati- 
tude he  was  near  the  end  of  the  month  of  May.  They 
saw  no  land  after  leaving  Hackluyt's  Headland  (or 
the  Northernmost  part  of  Spitzbergen,)  and  were 
back  in  the  month  of  June.  Did  not  find  the  cold 
excessive,  and  used  little  more  than  common  cloth- 
ing; met  with  but  little  ice,  and  the  less  the  far- 
ther they  went  to  the  Northward:  met  with  no  drift- 
wood. It  is  always  clear  weather  with  a  North  wind, 
and  thick  weather  with  a  Southerly  wind ;  neverthe- 
less they  could  take  the  sun^s  altitude  for  the  latitude 
most  days.  The  sea  is  quite  smooth  among  the  ice, 
as  in  the  river  Thames,  and  so  they  also  found  it  to 
the  North  of  Spitzbergen.  Met  with  no  ice  higher 
than  the  ship^s  gunnel.  Imagines  it  would  hardly 
have  been  colder  under  the  Pole  than  they  expe- 
rienced it;  although  he  thinks  the  cold  rather 
increased  on  going  Northward.  Thinks  the  currents, 
are  very  variable,  and  have  no  certain  or  constant 
direction.  Says  he  has  often  tasted  the  ice,  when 
the  sea  water  has  been  let  to  run  or  dry  off  it,  and 
always  found  it  fresh.  That  the  sea  water  will  freeze 
against  the  ship^s  bows  and  rigging,  but  he  never 
saw  it  freeze  in  the  ship.  That  it  never  freezes  in 
the  pumps.  A  little  piece  of  ice  detained  under  a 
large  piece  of  ice,  when  it  gets  loose  from  it  and 
^ornes  up  to  the  surface  of  the  water,  is  very  danger-^ 


^     I 


\ 


ON  APPROACHIirC 


1^. 


r 


ft 


^ 


ous,  it  emerging  with  a  force  which  will  sometimes 
knock  a  hole  in  the  bottom  of  the  ship.  The  Dutch 
ship  which  was  driven  with  theirs  from  Spitzbergen, 
ran  against  a  large  piece  of  ice,  and  was  lost,  the 
ships  being  therf  separated  to  a  considerable  dis- 
tance. The  winds  in  these  seas  are  generally 
Northerly ;  the  Southerly  winds  are  commonly  damp 
anl  cold." 

Having  thus  stated  the  memorandum  as  I  received 
it  from  Dr.  Maskelyne,  I  shall  now  make  some  obser- 
vations on  the  contents. 

It  appears  by  the  preceding  pages,  that,  in  this 
same  year,  viz.  1754,  both  Mr.  Ware  and  Mr.  Adams** 
sailed  to  82F  and  83°  during  the  month  of  June,  and 
both  of  them  conceived  that  they  might  have  reached 
the  North  Pole. 

Mr.  Maister,  by  letter  from  Hull,  dated  February 
24, 1777,  hath  procured  me  the  following  information 
from  a  friend  of  his,  who,  at  my  desire,  inquired  at 
Whitby  with  regard  to  any  ships  having  reached  high 
Northern  latitudes.     ^..        .  ^ 

"  Captain  Brown  of  the  Freelove  says,  that,  in  the 
year  1770,  he  was  certainly  in  82°  North  latitude, 
when  the  water  was  clear.  Captain  Cole  also  of  the 
Henrietta  says,  that  in  1776,  he  was  near  the  latitude 
of  81°  North,  and  afler  he  was  certain  of  being  in  th£^t 
latitude,  he  was,  with  strong  Southeast  gales,  drove 
for  three  days  to  the  Northward,  but  as  he  had  thick 

*  See  the  Probability  of  rebelling  the  North  Pole,  p.  42,  &c. 


weatherJ 
of  this  dj 

Itappj 
phens 
open  to  I 
year. 

Froi 

I  cannot 

early  in 

before  e 

the  CO 

rivers, 

sea,  it 

time  of 

rivers 

other  i 

bly  th< 

prece^ 

Ano 

1778, 

ed  at 

of  thi 

land 

ward 

same 

N< 

sians 

wha 

# 
and 


\\ 


r 

/ 


\ 


wMjfft*  a**^  ■"*'•*•"■  *"\1 


.tf-;^.-*!-. --_-..  ■ 


«i 


THE  NORTH  POLE. 


81 


kmetimes 
^e  Dutch 
Izbergen, 
Most,  the 
^ble  dis- 
[eneralljr 
yy  damp 


eceived 
'  obser- 

in  this 
^dams* 
ie»  and 
cached 

ibruary 
mation 
ired  at 
Jdhigh 


in  the 

itude, 

of  the 

titude 

nthf^t 

Jrove 

thick 

;c. 


weather,  the  distance  was  uncertain.    In  the  course 
of  this  drift  he  met  with  nothing  but  loose  ice.** 

It  appears  also  by  the  above  account,  that  Mr.  Ste- 
phens had  proceeded  as  far  as  84i%  the  sea  being 
open  to  the  Northward  a  month  earlier,  in  this  same 
year. 

From  this,  and  other  facts  of  the  same  kind, 
I  cannot  but  infer,  that  the  attempt  should  be  made 
early  in  the  season ;  if  I  am  right  also,  in  what  I  have 
before  supposed,  that  the  ice,  which  often  packs  near 
the  coasts  of  Spitzbergen,  comes  chiefly  from  the 
rivers,  which  empty  themselves  into  the  Tartarian 
sea,  it  seems  highly  probable,  that  this  is  the  proper 
time  of  pushing  to  the  Northward,  as  the  ice  in  such 
rivers  cannot  be  then  completely  broken  up.  What 
other  ice  therefore  may  be  seen  at  this  time  is  proba- 
bly the  remains  of  what  was  disembogued  during  the 
preceding  summer. 

Another  proof  of  this  arises  from  what  happened  in 
1778,  for  the  Carcase  and  Race  Horse  were  obstruct- 
ed at  80^%  by  an  immense  bank  of  ice,  during  part 
of  the  months  of  July  and  August;  but  four  Green- 
land Masters  were  a  degree  farther  to  the  North- 
ward during  the  months  of  May  and  June,  in  the 
same  year.* 

No  one  winters  in  Spitzbergen,  but  some  few  Rus- 
sians, from  whom  however  we  have  not  been  informed 
what  happens  during  that  season,  though  it  should 

*  See  the  Probability  of  reaching  the  North  Pole,  p.  4,  45,  4G, 
and  67. 

'      11        . 


# 


^J 


82 


ON  APPROACHING 


""S«C>Tf'^' 


It 
A' 


.«(«■ 


■tii 


\%- 


I' 


¥ 


Sv.em.  ft-om  the  observations  of  Barentz,  those  of  the 
Russians  in  Maloy  Brun,  and  a  ship  having  pushed  into 
the  Atlantic  from  Hudson's  Bay  during  the  midst  of 
December,*  that  the  Northern  Seas  are  then  navi- 
gable. 

For  the  same  reason,  probably,  Clipperton,t  who 
passed  the  Straits  of  Magellan  in  the  midst  of  winter, 
Haw  no  ice,  which  is  so  frequently  met  with  at  mid- 
summer by  those  who  sail  to  the  Southward  of  Cape 
Horn. 

I  take  this  opportunity  of  recapitulating  the  years 
bince  1746,:]:  during  which  it  appears,  from  the  in- 
stances I  have  stated,  that  the  sea  to  the  North 
of  Spitzbergen  hath  been  open,  so  as  to  permit 
attempts  of  approaching  the  Pole,  which  will  show 
tha*.  b.ch  opportunities  are  not  uncommon,  and  it  is 
hopedi  that  they  will  be  more  frequently  embraced, 
from  a  parliamentary  reward  of  five  thousand  pounds 
being  given  to  such  of  his  majesty's  subjects  as  shall 
first  penetrate  beyond  the  89th  degree  of  Northern 
latitude;  the  bill  for  which  purpose  hath  already 
passed  both  Houses  of  Parliament.^ 

*  See  tlie  Probability  of  reaching  the  North  Pole,  p.  83. 

t  Frezier  was  as  far  South  as  38°  in  the  middle  of  May,  and  saw 
no  ice,  though  he  speaks  of  a  Southeast  wind  as  cold. — See  Callan- 
der's Collection  of  Voyages^  vol.  iii.  p.  461. 
■     X  Viz.  1746,  1751,  1762,  1754,  1756,  1769,  17C3,  1765,  1766, 
1769,  1771,  and  1773. 

§  By  the  same  bill,  u  reward  of  twenty  thousand  founds  is  given  to 
such  of  his  majesty's  subjects  as  shall  first  discover  a  communication 
between  tfte  Atlantic  and  Pacific  Oceans,  in  any  direction  wbui- 
iioever  of  Ube  Northern  Hemisphere. 


^ 


4^  /■ 


* 


ie  of  the 

shed  into 

midst  of 

len  navi- 

^n,t  who 
^f  winter, 
at  mid- 
'  of  Cape 

he  years 
the  in- 
e  North 
0  permit 
^ill  show 
and  it  is 
nbraced, 
i  pounds 
!  as  shall 
Vorthem 
already 


r,  and  saw 
ee  Callau- 

r65,  1766, 

is  given  to 
nunicatioii 
ion  whai- 


Tlffi  NORTH  POLE. 


Ai  it  appears,  by  the  two  first  collections  of  in- 
stances, that  I  have  had  much  conversation  with 
the  officers  of  the  Royal  Navy,  as  well  as  masters 
of  Greenland  ships,  about  a  Polar  Voyage,  I  shall 
now  state  several  hints  which  have  occasionally 
dropped  from  them,  with  regard  to  prosecuting 
discoveries  to  the  Northward. 

The  ship  should  be  such  as  is  commonly  used  in 
the  Greenland  Fishery,  or  rather  of  a  smaller  size, 
as  it  works  the  more  readily  when  the  ice  begins  to 
pack  round  it. 

There  should,  on  no  account,  be  a  larger  com- 
plement of  men  than  can  be  conveniently  stowed  in 
the  boats,  a^  it  sometimes  happens,  that  the  Green- 
land vessels  are  lost  in  the  ice;  but  the  crews 
generally  escape  by  means  of  their  boats.  The 
crew  also  should  consist  of  a  larger  proportion  of 
smiths  and  carpenters  than  are  usually  put  on  board 
common  ships. 

As  it  may  happen,  that  the  crews  in  boats  may  be 
kept  a  considerable  time  before  they  can  reach 
either  ship  or  shore,  there  should  be  a  sort  of 
awning,  to  be  used  occuoionally,  if  the  weather  should 
prove  very  inclement. 

As  it  is  not  wanted  that  ihc  boats  should  last  many 
years,  it  is  advised,  that  they  should  be  built  of  the 
lightest  materials,  because,  on  this  account,  they 
are  more  easily  dragged  over  the  packed  ice.* 

*  General  Oglethorpe  informs  me,  that  the  Dutch  vessel.,  on  the 
Greenland  Fishery  have  three  boats  fastened  on  each  side  of  the 
tfhjp,  which  may  be  sufficient  to  contain  the  whole  «;i'ew  in  rase  of 


m^ 


m 


mt 


A  : 


m 


m 


# 


,:••<>.  sJilltp 


^-Tir;- 


■—*•-'"-•'-■-  *  "I'flff— ^  —  - 


81 


ON  APPROACHINO 


^ 


.#■ 


Si 


m 


n 


^  As  it  is  possible,  also,  that  the  crew  may  be 
obliged  to  M^inter  in  the  Arctic  Circle,  it  is  recom- 
mended, that  the  ship  should  be  ballasted  with  coals. 

That  there  should  be  a  framed  house  of  wood  on 
board,  to  be  made  as  long  as  possible,  for  the  oppor- 
tunity of  exercise  within  doors.* 

That  there  should  be  also  a  Russian  stove,  as  a 
fire  in  a  common  chimney  does  not  warm  the  room 
equably.  '^  .-- 

It  appears,  by  the  accounts  of  the  Dutch,  who 
wintered  in  Nova  Zembla,t  as  well  as  the  Russians, 
who  continued  six  years  in  Maloy  Brun,  that  during 
this  season  there  are  sometimes  days  of  a  tolerable 
temperature ;  snow  shoes,  therefore,  should  be  pro- 
vided, as  also  snow  eyes,  not  to  lose  the. benefit  of 
air  and  exercise  during  such  an   interval.|    The 

accidents ;  and  that  the  early  discoverers  had  alwa^  what  was  called 
a  ship  in  quarters  on  board,  which  might  be  put  together  when  a 
creek,  &c.  was  to  be  explored.  He  also  advises,  that  the  sailing  of 
the  two  ships,  to  be  sent  in  concert  on  discoveries,  should  be  pre- 
viously tried,  as  there  should  not  be  too  great  a  disparity  in  that 
circumstance. 

*  On  the  Labrador  Coast,  the  farriers  raise  a  wall  of  earth  all 
round  th«.a  '■  -i,  as  high  as  the  roof,  which  is  found  to  contribate 
much  to  warmth  within  doors,  so  as  to  want  little  more  heat  than 
arises  from  the  steam  of  lamps.  Such  wall  is  commonly  three  feet 
thick. 

t  The  Russian  Heretics,  of  the  old  faith,  as  they  are  styled, 
sometimes  winter  in  Nova  Zembla. — ^Account  of  Maloy  Brun. 

X  A  barrelled  organ,  which  plays  a  few  country  dances,  might 
amuse  during  the  dark  months,  as  also  be  of  use  in  the  first  inter- 
course with  the  savages,  music  being  a  sort  of  universal  language  ; 
and  Sir  Francis  Drake,  for  that  reason,  carried  out  musicians  with 
him.  ••:>       ■  1  ■  V5.V 


■'^i, 


^V. 


#' 


Jnr- 


-'■^ 


THE  NORTH  POLE. 


85 


[may  be 
recom- 

ih  coals. 

irood  on 
oppor- 

|v€,  as  a 
le  room 

ch,  who 
lussians, 
it  during 
olerable 
be  pro- 
enefit  of 
4    The 

was  called 
er  when  a 
e  sailing  of 
lid  be  pre* 
rityinthat 

f  earth  all 
contribute 
heat  than 
three  feet 


beard,  likewise,  should  be  suffered  to  grow  on  the 
approach  of  winter,  from  which  the  Russian  Cou* 
riers  are  enabled  to  support  the  severity  of  the 
open  air. 

Russian  boots,  and  the  winter  cap  of  the  furriers 
of  North  America,  are  also  recommended ;  but  re- 
course should  not  be  had  to  this  warmest  clothing 
upon  the  first  approach  of  winter,  for  by  these  means 
the  Russians  do  not  commonly  endure  cold  so  well  as 
the  English;  because,  when  the  weather  becomes 
excessively  severe,  they  cannot  well  add  to  their 
warmth.  • 

"When  the  weather  is  very  incknfbnt,  leads  for  the 
hands,  dumb-bells,  and  other  such  exercises,  should 
be  contrived  for  within-doors. 

In  order  to  prevent  the  scurvy,  likewise,  frequent 
use  of  the  flesh-brush  is  recommended,  as  also  occa- 
sionally a  warm  bath,  from  which  James's  crew 
received  great  benefit,  when  they  wintered  on  Charl- 
ton Island. 

With  regard  to  the  provisions,  I  shall  here  insert  a 
method  of  curing  meat,  communicated  to  me  by 
Admiral  Sir  Charles  Knowles,  the  good  effects  of 
which  both  himself  and  others  have  frequently  expe-^ 
rienced.* 


*n 


re  styled, 
>un. 

;es,  might 
irst  inter- 
language  ; 
ians  with 


^  So  soon  as  the  ox  is  killed,  let  it  be  skinned  and  cut  up  into 
pieces,  fit  for  use,  as  quick  as  possible,  and  salted  whibt  the  meat  is 
hot ;  for  which  purpose  have  a  sufficient  quantity  of  saltpetre  and 
bay  salt  pounded  together,  and  made  hot  in  an  oven,  of  each  equal 
parts  ;  with  this  sprinkle  the  meat,  at  the  rate  of  about  two  ounces 
to  the  pound.  Then  lay  the  pieces  on  shelving  boards  to  drain  for 
twenty  l-ar  hours;  which  done,  turn  them  and  repeat  the  same 


*i 


..W^' 


» 


\  M 


m^'' 


«»    HfUKii 


mShBI 


#       86 


ON  APPROAtllINO 


r.    -If!, 


i- 


II 


# 


^i. 


The  flour  Bliould  be  kiln-dried,  and  put  into  tight 
barrels  iii^hich  are  capable  of  holding  liquids.*  Flour 
thus  preserved  and  packed  hath  been  perfectly  good 
for  more  than  three  years,  without  the  least  appear- 
ance of  the  weevils. 

To  make  the  best  use  of  flour  thus  preserved, 
there  should  be  both  a  biscuit-maker  and  an  oven  on 
board. 

With  regard  to  liquors,  a  large  quantity  of  shrub 
from  the  best  spirits  and  fruits  is  recommehded, 
which  should  also  be  made  just  before  the  voyage 
takes  place ;  the  sg'onger  the  spirits,  the  less  stowage. 

operation,  and  let  them  lay  for  twenty  four  hours  longer,  by  whicli 
time  the  salt  will  be  all  melted,  and  have  penetrated  tlie  meat,  and 
the  juices  be  drained  off.  Each  piece  must  then  be  wiped  dry  with 
clean  coarse  cloths,  and  a  sufficient  quantity  of  common  salt,  made 
hot  likewise  in  an  oven,  and  mixed  (when  taken  out)  with  about  one* 
third  brown  sugar.  The  casks  being  ready,  rub  each  piece  well 
with  this  mixture,  and  pack  them  well  down,  allowing  half  a  pound 
of  the  salt  and  sugar  to  each  pound  of  meat,  and  it  will  keep  good 
several  years. 

N.  B.  It  is  best  to  proportion  the  casks  or  barrels  to  the  quantity 
consupaed  at  a  time,  as  the  more  seldom  the  meat  is  exposed  to  the 
air  the  better.  The  same  process  does  for  pork,  only  a  larger 
quantity  of  salt,  and  less  sugar ;  but  the  preservation  of  both  equally 
depends  on  the  meat's  being  hot  when  first  salted.  Sir  John  Nar- 
borough  salted  young  seals,  and  Sir  Richard  Hawkins  many  barrels 
of  penguins,  both  of  which  are  said  to  have  been  wholesome  and 
palatable  :  fish  likewise  caught  at  the  approach  of  winter,  might  be 
so  cured,  or  indeed  preserved  by  the  frost  without  any  salt.  Cap- 
tain Cook's  precautions  need  not  be  here  alluded  to. 

*  Woodes  Rogers  observes  in  his  voyage,  that  the  water,  which 
he  had  brought  with  him  from  England,  on  his  arrival  at  Juan 
Fernandez,  nas  all  spoiled  by  the  casks  being  bad.-Callander,  iiii 
p.  259. 


*4 


*•!' 


li— '    ■' 


/v 


4^ 


THE  NORTH  POLE. 


87 


^to  tight 
Flour 
t\y  good 
[appear- 

jserved, 
I  oven  on 

f  shrub 
mehded, 
;  voyage 
stowage. 

by  vvhicli 
meat,  and 
d  dry  with 
salt,  made 
about  one- 
piece  well 
Jf  a  pound 
keep  good 

le  quantity 
osed  to  the 
ly  a  larger 
>th  equally 
John  Nar- 
iny  barrels 
:some  and 
,  might  be 
alt.     Cap- 

ter,  which 
d  at  Juaa 
ander,  iii, 


Dampier  preferred  Vidonia  to  other  %vincs,  •  on 
account  of  its  acidity ;  and  perhaps  old  hock  might 
answer  still  better. 

I  should  stand  in  need  of  many  apologies,  for  hav- 
ing suggested  these  hints  to  Northern  Discoverers, 
had  I  not  received  them  from  officers  of  the  Royal 
Navy,  as  well  ub  Greenland  Masters,  and  eminent 
physicians;  if  any  of  these  particulars,  however, 
would  not  have  been  otherwise  thought  of  upon 
fitting  out  the  ship  for  such  a  voyage,  and  should  be 
attended  with  any  good  effects,  it  will  become  my 
best  excuse. 

Ill  order  also  to  promote  such  a  voyage  of  dis- 
covery, I  shou?d  conceive,  that  extending  the  Pariia- 
mentary  reward  of  twenty  thousand  pounds  by  18 
Geo.  II,  cap.  17,  for  the  passage  to  the  Pacific  Ocean 
through  Hudson's  Bay,  to  a  Northern  communication 
between  the  Atlantic  and  Pacific  Oceans  in  any 
direction  whatsoever,  might  greatly  contribute  to  the 
attempting  such  an  enterprise. 

To  this  another  incitement  might  perhaps  be  added, 
by  giving  one  thousand  pounds  for  every  degree  of 
Nor  h  latitude,  which  might  be  reached  by  the  adven- 
turer, from  85°  to  the  Pole,  as  some  so  very  perempto- 
rily deny  all  former  instances  of  having  penetrated 
to  such  high  latitudes.  An  act  hath  accordingly 
passed  for  the  first  of  these  purposes ;  and,  for  the 
second,  with  this  variation,  that  a  reward  of  five 
thousand  pounds  is  given  only  for  approaching  within 
a  degree  of  the  Pole. 

I  shall  conclude,  however,  in  answer  to  their  incre- 
dulity, by  the  following  citation  from  Hakluy  t : — 


X        -ti;' 


1 


1 

i 


4*? 


— -^^^ 


v\ 


i-iMM 


'^'*> 


% 


I . 


■  ! 

i 


88'  ON  APPROACHINO 

*^ow,  lest  you  should  make  tome  account  of 
ancient  writers,  or  of  their  experience,  who  travelled 
before  our  times,  reckoning  their  authority  amongst 
fables  of  no  importance,  I  have,  for  the  better  assur- 
ance of  those  proofs,  set  down  part  of  a  discourse 
written  in  the  Saxon  tongue,  and  translated  into 
English  by  Mr.  Nowel,  servant  to  master  Secretary 
Cecil,  wherein  is  described  a  navigation,  which  one 
Ochter  made  in  the  time  of  king  Alfred,  king  of  West 
Saxe,  anno  871 ;  the  words  of  which  discourse  arc 
these:  *He  sailed  right  North,  having  always  the 
desert  land  on  the  starboard,  and  on  the  larboard  the 
main  sea,  continuing  his  course  till  he  perceived  the 
coast  bowed  directly  towards  the  East,  &c.'  Where- 
by it  appeareth,  that  he  went  the  same  way  that  we 
do  now  yearly  trade  by  St.  Nicholas  into  Muscovia, 
which  no  man  in  our  age  knew  for  certainty  to  be 
nea,  till  it  was  again  discovered  by  the  English  in  the 
time  of  Edward  VI. 

«^  Nevertheless,  if  any  man  should  have  taken  this 
voyage  in  hand,  by  the  encouragement  of  this  only 
author,*  he  should  have  been  thought  but  simple, 

*  Perhaps  the  same  sea  is  alluded  to  in  the  following  line  of 
Dionysius : —  .  '  .»     • 

as  the  name  of  Frozen  can  scarcely  be  applied  to  that  of  the  Baltic. 

As  for  the  Thule  of  the  ancients,  about  which  so  many  conjec- 
tures have  been  made,  it  seems  most  clearly  to  have  been  Ireland, 
from  the  manner  in  which  Statius  addressed  a  Poem  to  Crispinus. 
whose  father  had  carried  the  Emperor's  commands  to  Thnle  : — 

tu  disce  patrem,  quantusque  nigrantem 

Flnctihva  occiduiSffeasoq.  Hyperione  ThvAen  "■ 

'•  Intra  vit  mant^afa  gerens.  '^^;- 


.s,> 


n 


.^  .t 


^'  &   ,4 


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ount  of 
ravelled 
amongst 
r  assur- 
iscourse 
ed  into 
iecretary 
hich  one 
of  West 
)ur8e  arc 
vays  the 
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Bived  the 
Where- 
r  that  we 
^uscovia, 
ntyto  be 
ish  in  the 

aken  this 
this  only 
t  simple, 

nng  lineof 


>*■ 


THE  NORTH  POLBi 


89 


^nsidering  that  this  navigation  was  written  so  manj 
years  past,  in  so  barbaroug  a  tongue,  by  one  only 
obscure  author;  and  yet  in  these  our  days,  we  find 
by  our  own  experience  his  reports  to  be  true/* 

It  should  aU»  seem,  from  other  parts  of  the  some  Poem,  that  thb 
General  had  croased  from  Scotland  to  the  North  of  Irelaad,  or 
Thule  :— 

Q^od  si  te  magno  tellus  franata  parenti 

Accipiat,  quantum  ferus  exultabit  Araxes  ? 

Qpanta  Caledonios  attollet  gloria  campos  ? 

Cum  tibi  longaems  referet  trucis  iucoln  terras, 

Ific  fuetus  dare  jura  parens,  hoc  cespite  turnlaa 

Affari ;  nitidas  speculas,  castellaque  long£. 

Aspidi  ?  ille  dedit  cinxitque  hac  moenia  fossil. 

Stativs,  r.  14. 
Crispinns's  father,  therefore,  must  have  resided  some  time  in  Scot* 
land,  from  whence  he  went  to  Thule  or  Ireland,  for  the  Hebrides 
(the  only  land  to  the  West  except  Ireland)  could  not  have  been  of 
sufficient  consequence  for  the  Emperor's  commission,  or  the  fortifi* 
cations  alluded  to  ;  besides  that  the  expression  oifeuoqut  Hyperione 
implies,  that  the  land  lay  considerably  to  the  Westward. 


.  %.  •  \Vi-:  ■ 


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the  Baltic, 
my  conjee- 
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THE  NORTH  POLE,* 


4i1    ' 
*■■■ 


XHE  possibility  of  making  discoveries  in  this  waj, 
(that  is,  by  steering  directly  North,)  though  now 
treated  as  paradoxical  by  many^  was  not,  as  will 
Hereafter  appear,  formerly  looked  upon  in  that 
light,  even  by  such  as  ought  to  be  reputed  the  pro* 
perlBBt  judges.  There  have  been  a  variety  of  causes, 
that,  at  different  times,  have  retarded  undertakings 
of  the  utmost  importance  to  the  human  species. 
Among  these  we  may  justly  consider  the  conduct  of 
some  great  philosophers,  who,  as  our  judicious  Veru- 
1am  wisely  observes,  quitting  the  luminous  path  of 
experience  to  investigate  the  operations  of  nature  by 
their  own  speculations,  imposed  upon  the  bulk  of 

*  I  have  lately  received  these  reflectiom  from  a  learned  friend, 
who  is  now  deceased,  and  who  permitted  me  to  print  them,  thoogh 
Dot  to  inform  the  puhlic  to  whom  they  ar*  indebted  for  this  very 
valuable  communication, 

D.  B ^— . 


*•?■ 


.'I* 


^. 


^ 


7  tj^Jf»-      ^** 


:SaBia:?»«sr- 


.x» 


» 


ON  APPROACHING 


U 


mankind  specious  opinions  for  incontestable  iruflis  ^ 
which)  being  propagated  by  theii?  disciples  through  a 
long  series  of  yearsj  captivated  the  minds  of  mea, 

\and  thereby  deprived  them  of  that  great  instrument 
of  science,  the  spirit  of  inquiry.*  In  spcceeding 
ages  a  new  impediment  arose,  from  the  setting  up 
profit  as  the  uhimate  object  of  discovery ;  and  then, 
as  might  well  be  expected}  the  preferring  the  private 
and  particular  gain  of  certain  individuals  to  the 
general  interests  of  the  community,  as  well  as  to 
the  interests  of  the  whole  world,  in  the  extension 
of  science.  This  it  was  that  induced  the  States 
General,  at  the  instance  of  their  East  India  Company, 
to  discourage  all  attempts  for  finding  a  Noftheast 
passage,  and  to  stifle  such  accounts  a9  tended  to 
show  that  it  was  practicable.  We  may  add  t<^ 
these,  the  sourness  of  disappointed  navigators,  who 
endeavoured  to  render  their  own  miscarris^es  proofs 
of  the  impracticability  of  any  like  attempts.  This 
was  the  case  of  Captain  Wood,  who  was  shipwrecked 
upon  Nova  Zembla^  and  who  declared,  that  all 
endeavours  on  that  side  were,  and  would  be  found 

^  vain;  though  Barentz,  who  died  there  in  a  like  expe- 
dition, a^rmed,  with  his  last  breath,  that,  in  his  own 
opinion,  such  a  passage  might  be  found.  ,     ,  ^  - 

That  the  earth  was  spherical  in  its  form  was  an 
opinion  very  early  entertained,  and  amongst  the 
learned  generally  admitted.  It  seemed  to  be  a  plain 
deduction  from  thence,  that  a  right  line,  passing 

*  Baconi  Opera,  torn.  iv.p.  IOC  ,  et  alibi  passim.  But  these  pas- 
sages may  be  found  collected  ia  Shaw's  Abridgment  '  Bacon's 
Works,  vol.  ii.  p.  62.  ■'    f    •^'  "- 


<js*. 


# 


le  trutlw  7 
through  a 
B  of  men. 
nstrument 
pcceeding 
setting  up 
and  then, 
le  private 
to  the 
veU  as  to 
extension 
he  States 
Company, 
Northeast 
tended  to 
ly  add  to 
itons,  who 
ges  proofe 
pts.    This 
ipwrecked 
)   that  all 
he  found 
like  expe- 
in  his  own 

^  was  an 
ongst  the 
^e  a  plain 
,  passing 

It  these  pes- 
*  Bacon's 


fHK  NORTlt  POClB.  W 

through  the  globe,  would  terminate  in  two  points 
diametrically  opposite.    Plato  is  thought  to  be  the 
first  who  spoke  of  the  inhabitants  (if  such  there  were) 
dwelling  at  or  near  those  points,  by  the  name  of 
Antipodes.   This  doctrine  occasioned  disputes  among 
))hilosophers  for  many  ages ;  some  maintained,  some 
denied,  and  some  treated  it  as  absurd,  ridiculous, 
and  impossible.*    Whoever  will  examine  impartially 
the  sentiments  of  these  great  men,  weigh  the  con- 
trariety of  their  opinions,  and  consider  the  singularity 
of  their  reasonings,  will  see  and  be  convinced  how 
unsatisfactory  their  notions  were,  and  discover  from 
thence,  how  insufficient  the  subtle  speculations  of  the 
human  understanding  are  towards  settling  points  like 
these,  when  totally  unassisted  by  the  lights  of  ob- 
servation and  actual  experience. 
'  The  division  of  the  globe  by  zones  being  agreeable 
to  nature,  the  ancients  distinguished  them  very  pro- 
perly and  accurately  into  two  frigid,  the  Arctic  and 
Antarctic  Circles ;    two  temperate,  lying  between 
those  circles  and  the  tropics;  and  the  torrid  zone 
within  the  tropics,  equally  divided  by  the  equinoctial. 
But  judging  from  their  experience  of  the  nature  of 
the  climates  at  the  extremities  of  the  zone  which 
they  inhabited,  they  concluded,  that  the  frigid  zones 
were  utterly  uninhabitable  from  odd,  and  tlie  torrid 
from  intolerable  heat  of  the  sun.    Pliny  laments  very 
pathetically  upon  this  supposition,  that  the  race  of 

*  Lucr.  de  Natura  Rerutn,lib.  i.  ver.  1063 ;  Cicer.  Acad.  Qjniest. 
lib.  It.  ;  Plin.  Hist.  Nat.  lib.  ii.  cap.  65 ;  Pint,  de  Fncic  in  Orhe 
Laaae ;  Macrob.  de  Soma.  Scip.  lib.  i^ 


I 


■t 


'T 


4 


K>t  jKllirj  w'iBW*fet!^ 


..^ 


l;i-38Kir»"«r* 


( 


a 


« 


ON  APPROACHflVO 


mdtikind  were  pent  up  in  so  snUeJl  a  piart  of  th«  eartli.' 
The  poets,  who  were  also  no  despicable  philoso* 
phers,  heightened  the  horrors  of  these  inhospitable 
iregfons  by  all  the  colooring  of  a  warm  HdA  heated 
imagination;*  but  we  now  know,  with  the  utmoA 
certainty,  that  they  were  entirely  mistaken  as  if 
both.  For  within  the  Arctic  Circle  there  *  are  coun* 
tries  inhabited  as  high  nearly  as  we  have  discovered  f 
and,  if  we  may  confide  in  the  relations  of  those  who 
have  been  nearest  the  PoIe,t  the  heat  there  is  very 
considerable,  in  respect  to  which  our  own  navigators 
and  the  Dutch  perfectly  i^ee.  .In  regard  to  the 
torrid  zone,  we  have  now  not  the  lieast  doubt  of  its 
being  thoroughly  inhabited ;  and,  which  is  mor6 
WQndeHul,  that  the  climates  are  very  different  there, 
according  to  the  circumstances  of  their  situation.  In 
Ethiopia,  Arabia,  and  the  Moluccas,  .exceedingly 
hot;  but  in  the  plains  of  Peru  (and  particularly  at 


f. 


f 


m 


*  Cicero  in  Soranium  Sciopinis ;  Virg.  Geoig.  lib.  i. ;  Ovidii  Met* 
lib.  i. ;  Tiballus  Panegyr.  ad  Messalam,  lib.  iv. ;  Plin.  Hist  Nat. ' 
lib.  ii.  cap.  68;  Pomp.  Mela  de  Situ  Orbis,  lib.  i.  cap.  1  ;  Claude 
de  Raptu  Proserpinae,  lib.  i. 

t  That  the  <iarth  had  inhabitants,  even  under  the  Poles,  seems  to 
l^are  been  beUeved  by  many  at  the  latter  end  of  the  sixteenUi  cen* 
tury,  from  the  following  lines  :■-- 

"  Fond  men!  if  we  believe  that  men  do  livd    ' 
Undef  the.  zenith  of  both  frozen  poles ; 
Though  none  come  thence  advertisements  to  give, 
Why  bear  we  not  the  like  faith  of  our  souls  ?" 
i  ^^^  John  Davis's  ^osce  te  ipsutHf 

Probably  written  in  1596,  from  a  complunentto  Lord  Keeper  Eger* 
ton  on  hii  first  receiving  the  Great  S^al. 

^,'..-^        v,  B  I .. 


'^.• 


^--.. 


BMfttllt.l  I' '.' * 


ftm  NORTH  POLS. 


»d 


liilicflrdi.' 

philoso- 

ospitable 

ft  iMMteA 

Qtmodt 

sn  M  i^ 

ure  coun* 

icovered  i 

lose  who 

■e  is  very 

lavig&iors 

■d  to  the 

abt  of  ltd 

is  more 

ent  there^ 

atioh.    In 

ceedSngljr 

icularly  at 

OvidiiMet. 
.  Hist  Nat. 
.  1 ;  Cbud. 

les,  seems  to 
cteenUi  cen« 


ive, 

» 

•  te  ipsum, 
eeperEger*  ' 

B .. 


Quito)  perfectly  temperate,  so  that  die  inhabitants 
never  change  their  clothes  in  any  season  of  t|ie  year. 
Thf  sentiments  of  the  ancients  therefiure  in  this 
respect  are  a  proof  ho.w  inadequate  the  Acuities  of 
the  human  mind  ajre  to  discussions  of  this  nature* 
nrhen  unasEHsted  by  facts. 

t  TliA  Pythagorean  system  of  the  universe,  revised 
and  restored  near  two  hundred  and  fifty  years  ago 
by  tb€  celebrated  Copernicus,  met  with  a  very  diffi* 
cult  and  slow  reception,  not  only  from  the  bulk  of 
mankind,  for  that  might  have  been  well  expected, 
but  even  from  the  learned;  and  some  very  able 
astronomers  attempted  to  overturn  and  refute  it*' 
Qnlileo  Galilei  wrote  an  admirable  treaties  in  its 
support,  in  which  he  very  fuUy  removed  most  of  the 
popular  objection8.t  This,  however,  exposed  him 
to  the  rigour  of  the  inquisition,  and  he  was  obliged 
to  abjure  the  doctrine  of  the  earth*s  motion.  Our 
noble  plulosopher,  the  deep  and  acute  Lord  Veru- 
1am,  could  not  absolutely  confide  in  the  truth  and 
certainty  of  the  Copemican  System;  but  seems  to 
think,  that  its  facilitating  astronomical  calculations 
was  its  principal  recommendation,  as  if  this  had  not 

*  Amongst  the  most  considerable  of  these  was  John  Baptist  Ric< 
cioli,  who  published  his  A^magestum  JVovtim  with  this  view.  Yet 
afterward,  in  his  Aitronomia  Reformata^  he  found  himself  obliged  to 
havie  recourse  te  the  doctrine  of  the  earth's  motion,  that  he  might 
be  able' to  fivje  his  calculations  with  a  proper  degree  of  exactness. 

t  This  celebrated  work  of  his  was  entitled,  Dialoghi  de  Sistemi  di 
Tolomeo,  e  di  Copemieo.  This  is  much  better  known  to  the  learned 
worid  by  a  Latin  translation,  which  so  clearly  proved  the  superiority 
of  the  Copemican  System,  that  the  only  means  of  refuting  it  was  by 
the  censures  of  the  Church. 


\ 


») 


-^■i 


«> 

^ 


^ 


09 


ON  APPROACHIKtl 


4 


r 


(■-r 


^  * 


beert  also  a  very  strong  presumption  at  least,  if  not  a 
prooff  of  its  veracity.*  .It  was  from  this  consideration 
that  the  church  of  Rome  at  length  thought  fit  so  far 
to  relax  in  her  decisions,  as  to  permit  the  maintain- 
ing  the  earth*s  motion  in  physical  and  i^ilosophical 
disquisitions.  But  Sir  Isaac  Newton,  who  built  upon 
this  basis  his  experimentsd  philosophy,  hath  dispersed 
all  doubts  on  this  subject^  and  shown  how  the  most 
•ublime  discoveries  may  be  made  by  the  reci];>rocal 
aids  of  sagacity  and  observation.  On  tiiese  grounds, 
therefore,  all  inquiries  of  this  nature  ought  to  pro- 
ceed, widiout  paying  an  implicit  submission  to  the 
mere  speculative  notions  even  of  the  greatest  men ; 
but  pursuing  steadily  the  path  of  truth,  utader  the 
direction  of  the  li|^t  of  experience.  ^ 

It  may  be  Tirged,  in  excuse  of  the  ancients,  and 
even  of  our  ancestors  of  former  times,  that,  as  they 
were  unassisted  by  facts,  they  could  onlj  employ 
guess  and  conjecture,  and  that  consequently  Uieir 
conclusions  were  from  thence  erroneous.  But  to 
waive  the  visible  impropriety  of  decicling  in  points, 
where  observation  was  so  obviously  necessary  with- 
out its  direction ;  let  us  see  whether  this  plea  of  alle- 
viation may  not  be  controverted  in  both  cases. 
Cornelius  Ncpos  reports,  that  some  Indians  being  cast 
on  shore  in  Germany  were  sent  by  a  prince  of  the 
Suevi  to  Quintus  MeteUus  Celer,  then  the  Roman 
proconsul  in  GauLf    A  very  learned  writer,  in  dis- 


,4 


I 


r» 


f  Shaw*8  Abridgment  of  Bacon's  Worlcs,  vol.  ii.  p.  21.  where 
the  Doctor  endeavours  to  defend  this  opinion. 

t  Plin.  Hist.  Nat.  lib.  ii. xag,  67.  -  .•'^• 


I. 


•  t    I 


it  'i 


I   i 


THE  NORTH  POLE. 


if 


>tf  if  not  a 
lideration 
fit  so  far 
maintain- 
losophical 
>uilt  upon 
disperaed 
the  most 
eci^rocal 
grounds, 
;ht  to  pro- 
on  to  the 
itest  men ; 
under  the 

:ients,  and 
Sit,  as  they 
ly  employ 
ently  Uieir 
fe^But  to 
in  points, 
ssarywith- 
leaofalle- 
Dth  cases, 
being  cast 
ice  of  the 
le  Roman 
er,  in  dis- 

p.  21.  where 


I: 


ff 


cussing  this  point,  hath  shown,  that  it  was  possible 
for  these  Indians  to  have  come  by  two  difierent  routes 
into  the  Baltic.    He  thinks,  however,  that  it  is  very 
improbable  they  came  by  either,  and  supposes,  that 
they  were  either  Norwegians,  or  some  other  wild 
people,  to  whom,  from  their  savage  appearance,  they 
gave  the  name  of  Indians.*    But  though  this  observa- 
tion may  well  enough  apply  to  the  Romans,  who  at 
that  time  had  no  knowledge  of  these  Northern  peo- 
ple, yet  it  is  not  easy  to  conceive  that  the  Suevi 
*^ould  fall  into  this  mistake ;  or,  if  they  did  not,  that 
they  should  attempt  to  impose  upon  the  Romans.     It 
appears  incontestably,  that,  in  the  time  of  King  Alfred, 
the  Northern  seas  were  constantly  navigated  upon 
the  same  motives  they  are  now ;  that  is,  for  the  sake  . 
of  catching  whales  and  sea-horses.t    Nicholas  of 
Lynn,  a  Carmelite  Friar,  sailed  to  the  most  distant 
islands  in  the  North,  and  even  as  high  as  the  Pole. 
He  dedicated  an  account  of  his  discoveries  to  King 
Edward   the  Third,  and  was  certainly  a  person  of 
great  learning,  and  an  able  astronomer,^  if  we  may 

*  Hnet  Histoire  de  Commerce,  et  de  la  Navigation  des  Anciens, 
p.  631. 

t  See  Barrington's  Translation  of  Orosius  from  the  Anglo-Saxon 
of  King  Alfred,  part  ii.  p.  9. 

X  Leland.  Comment,  de  Script.  Britan.  cap.  370  ;  Bale,  vi.  25  ; 
Pits,  p.  605.  His  description  was  intituled  Inventio  FortuTiata; 
besides  which,  he  wrote,  amongst  other  things,  a  book,  De  Mundi 
Revolutione,  which  possibly  may  still  remain  in  the  Bodleian  Library. 
This  Friar,  as  Dr.  Dee  asserts,  made  five  voyages  into  these  North- 
ern parts,  and  left  an  account  of  his  discoveries  from  the  latitude 
of  64' to  the  Pole. 

13 


%       # 


^ 


V(i 


ir.-l 


i.^.       S^A 


% 
■^ 


.-*.. 


90 


ON  APPBOAOHING 


believe  the  Celebrated  Chaucer,  who,  in  his  Treatise 
on  the  Astrolabe,  mentions  him  with  great  respect. 

After  Columbus  discovered  America,  under  the 
auspices  of  Ferdinand  and  Isabella,  the  Sovereigns 
of  Europe,  and  especially  Henry  the  Seventh,  turned 
their  thoughts  towards,  and  gave  great  encourage^ 
ment  to,  discoveries.  Mr.  Robert  Thome,  who  resided 
many  years  as  a  merchant  in  Spain,  and  who  was 
afterward  mayor  of  Bristol,  wrote  a  letter  to  Henry 
the  Eighth,  in  which  he  strongly  recommended  a 
voyage  to  the  North  Pole.  He  gave  his  reasons* 
more  at  large  in  a  long  Memorial  to  our  ambassador 
in  Spain,  which  show  him  to  have  been  a  very  judi- 
cious man,  and  for  those  times  a  very  able  cosmogra- 
pher;  and  accompanied  this  Memorial  with  a  map 
of  the  world,  to  prove  the  practicability  of  his  pro- 
posaL*"  Though  this  project  of  his  was  not  attended 
to,  yet  a  variety  of  expeditions  were  made  for  disco- 
vering  a  passage  by  the  Northwest,  and  others  by  the 
Northeast,  into  the  South  seas  on  the  one  side,  and 
into  the  Tartarean  ocean  on  the  other,  until  at  length 
both  were  declared  impracticable  by  Captain  James 
and  Captain  Wood;  soured  by  their  own  miscar- 
riages, and  being  strongly  persuaded,  that,  as  they  did 
not  succeed,  none  else  could.  But  even  these  unsuc- 
cessful voyages  were  not  unprofitable  to  the  nation 
upon  the  whole,  as  they  opened  a  passage  to  many 
lucrath^e  fisheries,  such  as  those  in  Davis's  Straits, 

*  Haklujrt's  Voyiges,  vol.  i.  p.  212—220.  The  letter  to  Dr. 
Ley,  who  was  the  King's  Ambassador  in  Spain,  is  dated  A.  D. 
1627.  This  Mr.  Thome's  father  waa  engaged,  with  others,  in  the 
discovery  of  Newfoundland. 


# 


'■^"ir' 


THE  KORTH  POLE. 


99 


his  Treatise 
|at  respect, 
under  the 
Sovereigns 
renth,  turned 
encourage- 
who  resided 
id  who  was 
|ter  to  Henry 
tmmended  a 
his  reasons' 
'  ambassador 
a  very  judi- 
le  cosmogra> 
with  a  map 
Y  of  his  pro- 
not  attended 
de  fordisco- 
)tbers  by  the 
ne  side,  and 
ntil  at  length 
ptain  James 
own  miscar- 
t,  as  thejr  did 
these  unsuc- 
0  the  nation 
?e  to  manj 
^is's  Straits, 

B  letter  to  Dr. 
8  dated  A.  D. 
others,  m  the 


Baffin's  Bay,  and  on  the  coast  of  Spitzbergen. 
Besides  this,  they  laid  open  Hudson's  Straits  and  Bay, 
with  the  coast  on  both  sides,  which  have  been  alrea- 
dy productive  of  many  advantages,  and  which,  in 
process  of  time,  cannot  fail  of  producing  m^oi^,  in 
consequence  of  our  being  in  possession  of  Canada,  and 
being  thereby  sole  master  of  those  seas  and  coasts. 

It  is,  however,  very  remarkable,  that  notwithstand- 
ing the  views,  both  of  our  traders  and  of  such  great 
men  as  were  distinguished  encouragers  of  discove- 
ries, the  ablest  seamen  (who  without  doubt  are  the  - 
best  judges)  were  still  inclined  to  this  passage  by 
the  North,  such  as  Captain  Poole,  Sir  William  Moil* 
son,'*  and  others ;  and  this  was  still  the  more  remark- 
able, as  they  were  entirely  guided  therein  by  the 
lights  of  their  own  experience,*>'having  no  knowledge 
of  Mr.  Thome's  proposal,  or  of  the  sentiments  of 
each  other.  From  the  reason  of  the  thing,  however, 
they  uniformly  concurred  in  the  motives  they  sug- 
gested for  such  an  undertaking.  They  asserted,  that 
this  passage  would  be  much  shorter  and  easier  than 
any  of  those  by  the  Northwest  or  Northeast;  that  it 
would  be  more  healthy  for  the  seamen,  and  attended 
with  fewer  inconveniences;  that  it  would  probablj 
open  a  passage  to  new  countries ;  and,  finally,  that 
the  experiment  might  be  made  with  very  little  hazard, 
at  a  small  expense,  and  would  redound  highly  to  our 
national  honour,  if  attended  with  success.  It  may 
be  then  demanded,  why  it  has  not  hitherto  been  at- 
tempted, and  what  objections  have  retarded  a  scheme 


-  '■'■\f 


A' J      S:-:-'-'. 


*  Naval  Tracts,  p.  435. 


* 


0 


100 


ON  APPMACHIIfO 


# 


k. 


SO  visibly  advantageous  ?  These  objections^  as  far 
as  they  can  be  collected,  are  the  fear  of  perishing  by 
excessive  cold,  the  danger  of  being  blocked  up  in 
ice,  and  the  apprehension  that  there  could  be  no 
certainty  of  preserving  the  use  of  the  compi^is  under 
or  near  the  Pole. 

In  respect  to  the  first,  we  have  already  mentioned, 
that  the  ancients  had  taken  up  an  opinion,  that  the 
seas  in  the  frigid  zone  were  impassable,  and  the 
lands,  if  there  were  any,  uninhabitable.  The  phi- 
losophers of  later  ages  fell  into  the  same  opinion,  and 
maintained  that  the  Poles  were  the  sources  and  prin- 
ciples of  cold,  which  of  course  increased  and  grew 
excessive  in  approaching  them.''^  But  when  the 
lights  of  experience  were  admitted  to  guide  in  such 
researches,  the  truth  6i  this  notion  came  to  be  ques- 
tioned, because  from  facts  it  became  probable,  that 
there  might  be  a  diversity  of  climates  in  the  frigid 
as  well  as  in  the  torrid  zone.  Charlton  Island,  in 
which  Captain  James  wintered,  lies  in  the  bottom, 
that  is,  in  the  most  Southern  part  of  Hudson^s  Bay, 
and  in  the  same  latitude  with  Cambridge,  and  the 
cold  there  was  intolerable.  The  servants  of  the 
Hudson^s  Bay  Company  trade  annually  in  places  ten 
.,.,,  degrees  nearer  the  Pole,  without  feeling  any  such 
inconvenience.  The  city  of  Moscow  is  in  the  same 
latitude  with  that  of  Edinburgh,  and  yet  in  winter 
the  weather  is  almost  as  severe  there  as  in  Charlton 

*  In  the  language  of  those  times,  the  Pole  was  styled  Primvm 
J     Frigidum ;  and  it  was  by  such  groundless  phrases  that  men  pre^ 
tended  to  account  for  the  operations  of  nature,  without  giving  them- 
telves  the  trouble  of  experimental  inquiries. 


THE  NORTH  POLE. 


101 


Dns,  as  far 
^riuhing  by 
eked  up  in 
>uld  be  no 
[pa^fs  under 

mentioned, 
>n,  that  the 
le,  and  the 
The  phi- 
pinion,  and 
s  and  prin- 
d  and  grew 
when   the 
ide  in  such 
to  be  ques- 
bable,  that 
the  frigid 
1  Island,  in 
he  bottom, 
dson's  Bay, 
;e,  and  the 
ints  of  the 
places  ten 
5  any  such 
n  the  same 
t  in  winter 
Q  Charlton 

tyled  Pritnutn 

iat  men  pre-. 

giving  tbeiq- 


Island.  Nova  Zembla  hath  no  soil,  herbage,  or^ni- 
mals ;  and  yet  in  Spitzbergen,  in  six  degrees  higher 
latitude,  there  are  all  three ;  and,  on  the  top  of  the 
mountains  in  the  most  Northern  part,  men  strip  them- 
selves of  their  shirts  that  they  may  cool  their  bodies.* 
The  celebrated  Mr.  Boyle,  from  these  and  many 
other  instances,  rejected  the  long-received  notion, 
that  the  Pole  was  the  principle  of  cold.  Captain 
Jonas  Poole,  who  in  1610  sailed  in  a  vessel  of  seventy 
tons  to  make  discoveries  towards  the  North,  found 
the  weather  warm  in  near  79**  of  latitude,  whilst 
the  ponds  and  lakes  were  unfrozen,  which  put  him 
in  hopes  of  finding  a  mild  summer,  and  led  him  to 
believe,  that  a  passage  might  be  as  soon  found  by  the 
Pole  as  any  other  way  whatever ;  and  for  this  reason, 
that  the  sun  gave  a  great  heat  there,  and  that  the  ice 
was  not  near  so  thick  as  what  he  had  met  with  in 
the  latitude  of  TS^'.t  Indeed,  the  Dutchmen,  who 
pretend  to  have  advanced  within  a  degree  of  the 
Pole,  said  it  was  as  hot  there  as  in  the  summer  at 
Amsterdam. 

*  In  these  Northern  Voyages  we  hear  very  much  of 
ice,  and  there  is  no  doubt  that  vessels  are  very  much 
hindered  and  inconmioded  thereby.  But  after  all,  it 
is,  in  the  opinion  of  able  and  experienced  seamen*, 
more  formidable  in  appearance  than  fatal  in  its 
effects.  When  our  earliest  discoveries  were  made, 
and  they  reached  farther  North  than  we  commonly 
.»..     pail  at  present,  it  was  performed  in  barks  of  seventy 

W  •  See  Marden's  Account  of  Spitzbergen,  p.  105. 

t  Purchas'e  PilgriiQg,  vol.  iii.  p.  702. 


i 


.A 


4 


1^ 


I- 


I 


♦ 


^^M 


102 


ON  APPROACHING 


ton^  with  some  trouble,  no  doubt,  but  with  very  little 
hazard.  At  this  <^ay  it  is  known,  that  in  no  part  of 
the  world  there  are  greater  quantities  of  ice  seen 
than  in  Hudson^s  Bay,  and  yet  there  is  no  navigation 
safer,  the  company  not  losing  a  ship  in  twenty  years, 
and  the  seamen,  who  are  used  to  it,  are  not  troubled 
with  any  apprehensions  about  it.  It  is  no  objection 
to  this,  that  we  hear  almost  every  season  of  ships  lost 
in  the  ice  on  the  Whale  fishery;  for  these  vessels, 
instead  of  avoiding,  industriously  seek  the  ice,  as 
amongst  it  the  whales  are  more  cmnmonly  found  than 
in  the  open  sea.  Being  thus  continually  amongst  the 
ice,  it  is  no  wonder  that  they  are  sometimes  surround- 
ed by  it;  and  yet  the  men^  when  the  ships  are  lost,  gene- 
rally speaking,  escape.  But  in  the  seas  near  the  Pole, 
it  is  very  probable  there  is  little  or  no  ice,  for  that  is 
commonly  formed  in  bays  and  rivoi3  during  winter, 
and  does  not  break  up  and  get  into  the  sea  till  the 
latter  end  of  March,  or  the  beginning  of  April,  vdien 
it  begins  to  thaw  upon  the  shores.  It  is  aIso»  when 
formed,  very  uncertain  as  to  its  continuance,  being 
broken  and  driven  about  by  the  vehemence  of  the 
winds.  As  a  proof  of  this  we  have  an  instance  of  a 
vessel  fi'ozen  in  one  of  the  harbours  of  Hudson^s  Bay, 
^  which,  by  the  breaking  of  the  ice,  drove  to  sea,  and, 
'  though  it  was  Christmas,  found  the  Straits  quite  free 
from  ice,**^  which  are  frequently  choked  with  it  in  May 
and  June,  and  made  a  safe  and  speedy  passage  home. 
All  our  accounts  agree,  that,  in  very  high  latitudes, 
there  is  less  ice.  Barentz,  when  his  ship  was  frozen  in 


R  ■ 


Mr.  Dobb's  Account  of  Hudson's  Bay,  p.  69,  70. 


w 


THE  NORTH   POLE. 


103 


l: 


e 


very  little 
ID  part  of 
ice  seen 
lavigation 
nty  years, 
troubled 
objection 
ships  lost 
vessels, 
ice,  as 
rand  than 
longst  the 
Burround- 
<tot,gene- 
thePole, 
for  that  is 
g  winter, 
»  till  the 
ril,  when 
lso»  when 
ce,  being 
:e  of  the 
ince  of  a 
on's  Bay, 
sea,  and, 
[uite  free 
it  in  May 
^  home, 
atitudes, 

frozen  in 

:''    :    _  •      ■# 

0. 


■•t«* 


Nova  2.-^mbla,  heard  the  ice  broken  with  a  most 
horrible  noise  by  an  impetuous  sea  from  the  North, 
a  full  proof  that  it  was  open.  It  is  the  invariable 
tradition  of  the  Samoides  and  Tartars,  who  live 
beyond  the  Waygat,  that  the  sea  is  open  to  the 
Ncrth  of  NovaZembla  all  the  year;  and  the  most 
knowing  people  in  Russia  are  of  the  same  opinion. 
The&e  authorities  ought  certainly  to  have  more 
weight  than  simple  conjectures. 

The  notion,  that  approaching  to  a  passage  under 
the  Pole  would  destroy  the  use  of  the  compass,  is  a 
popular  opinion  without  any  just  grounds  to  support 
it.  For  it  presumes  that  the  needle  is  directed  by 
the  Pole  of  the  World ;  which  it  certainly  is  not,  as 
appears  from  the  needless  variation,  and  even  the 
variation  of  that  variation,  which,  if  this  notion  was 
true,  could  never  happen.  In  Sir  Thomas  Smithes 
Sound  in  Baffin^s  Bay.,  the  variation  was  found  to  be 
d6**  Westward,  the  greatest  yet  known.  Captain 
Wood  is  veiy  clear  upon  this  point,  and  maintains, 
^that  no  danger  was  to  be  apprehended  from  this 
cause.**  Those  who  asserted,  that  they  had  advanced 
within  a  degree  of  the  Pole,  estimated  the  variation 
there  at  five  points  of  the  compass.  Captain  Wood, 
in  stating  the  account  given  of  the  Dutch  seamen's 
voyage  by  Captain  Goulden,  omits  one  very  material 
point,  of  which  we  are  informed  by  Mr.  Boyle,  which 
is,  that  one  of  the  Dutch  captains  coming  over  to 
England,  Captain  Goulden  carried  him  to  some  of 
the  Northern  Company,  who  were  perfectly  satisfied 

*  Wood's  Voyage  for  the  Discovery  of  a  Northeast  Passage, 
p.  139 


r 


\' 


J  '-i 


'^-:J-/^""-S!r,---  *■.  ■*- 


iH 


V, 


ON  APPROACHING 


as  to  the  truth  of  his  relation.*  On  the  whole,  there- 
fore, whether  we  respect  reason  or  facts,  there  are 
no  just  grounds  for  apprehensions  on  this  head,  more 
especially  as  there  are  other  means  by  which  the 
true  situation  of  a  vessel  might  be  determined,  and 
the  difficulty,  if  any  arose,  would  be  but  of  very 
short  continuance.  But  as  such  a  voyage  could  not 
fail  of  affording  many  new  lights  in  respect  to  astro- 
nomy and  geography,  so  in  this  respect  also  it  must 
necessarily  ascertain  fully  what  is  at  present  only 
ma,tter  of  doubt  and  conjecture. 

As  notions  long  received  acquire  from  thence  a 
degree  of  credit  due  only  to  tpith ;  and  as  new 
opinions,  contrary  to  these,  and  in  other  respects 
perhaps  extraordinary  in  themselves,  meet  from  these 
causes  with  slow  and  difficult  belief,  however  they 
may  appear  to  be  supported  by  arguments,  authori- 
ties, or  facts,  (which  it  is  presumed  have  been  freely 
and  fairly  urged  in  the  present  case,  to  a  degree  that 
may  at  least  entitle  the  matter  to  ^ome  attention) 
let  us  now  proceed  one  step  farther.  This  shall  be 
to  show,  that  what  seems  to  be  so  repugnant  to  the 
common  course  of  things  (viz.  that  near  the  North  Pole 
the  cold  should  releuc,  and  the  ice  be  less  trouble- 
.fiome)  is  perfectly  conformable  to  the  laws  of  nature, 
or,  which  is  the  same  thing,  to  the  will  and  wisdom 
of  our  great  Creator.  If  this  can  be  proved,  there 
can  be  no  farther  dispute  as  to  the  possibility  of  this 

*  See  the  honourable  Mr.  Boyle's  History  of  Cold,  in  respect  to 
this  and  a  multitude  of  other  curious  particulars,  which  show  with 
how  much  industry  and  care  he  struggled  to  deliver  truth  from  vu^    ^ 
gar  errors  and  fiction. 


TNIi  NORTH  FOI.K. 


10$ 


|e,  there- 
lere  are 
id,  more 
lich  the 
led,  and 
of  very 
bould  not 
I  to  astro- 
it  must 
Jent  only 

thence  a 
as  new 

respects 

om  these 
iver  they 

authori- 
jen  freely 
gree  that 
ittention) 

shall  be 
nt  to  the 
orthPole 

trouble- 
f  nature, 
1  wisdom 
>d,  there 
y  of  this 

respect  to 

show  with 

from  vu|r 


passage  I  more  especially  vben  it  shall  also  appear* 
that  this  afibids  a  fbll  solution  of  all  the  doubts  that 
have  been  suggested,  and  at  the  same  time  clearly 
accounts  for,  and  effectually  confirms,  the  tacts  and 
reasonings  deduced  from  them,  which  have  been 
already  advanced  upon  this  subject.  To  qome  then 
at  once  to  the  point. 

Sir  Isaac  Newton*  who  it  is  universally  allowed 
was  equally  accurate,  cautious,  and  judicious,  in  his 
philosophical  decisions,  hath  demorsirated  clearly, 
that  the  figure  of  this  our  earth  is  not  sphericalf  but 
of  an  oblate  spheroidal  form*  the  diameter  at  the 
equator  being  the  greatest,  and  at  the  ai^is  the  least 
of  all  the  lines  that  can  pass  through  the  centre. 
He  also  determined,  by  a  most  cUrious  calculation? 
the  proportion  of  these  diameters  to  be  as  two 
hundred  and  thirty  to  two  hundred  and  twenty'^nine. 
These  sentiments  of  his  have  been  experimentally 
verified  by  the  means  which  he  also  pointed  out,  viz. 
observing  the  motion  of  pendulums  in  very  diflferent 
latitudes,  and  the  actual  measurement  of  a  degree  at 
the  Equator  and  under  the  Arctic  Circle.  This  last 
evidently  proved  the  depression  of  the  earth's  sur- 
face towards  the  Pole,  which  no  doubt  gradually 
increases.  The  very  learned  and  sagacious  Dr. 
Hooke  asserted,  in  one  of  his  lectures,  and  brought 
very  strong  reasons  to  show,  that  there  is  nothing 
but  sea  at  the  Poles.*  These  points  then,  being 
maturely  considered,  will  be  found  to  militate  in 
fyvour  of  a  free  passage  this  way,  and  at  the  same 


?<{«■ 


♦  Hooke's  Posthumous  Works,  p.  351. 
'V  14 


*^' 


m. 


*u 


^  >.  - 


*ii  ••«>'- --w 


■r- 


^•^. 


106 


ON  APPROACHING 


time  give  much  light  into  other  things  that  have  been 
advanced  in  the  course  of  this  inquiry,  by  showing 
the  true  causes  of  those  facts  that,  at  first  sight,  have 
appeared  to  many  very  strange  and  unaccountable. 
For  example,  if  there  be  no  land  near  the  Pole,  then 
there  can  be  no  bays  in  which  ice  can  be  formed  to 
interrupt  the  navigation.  Again,  the  rays  of  the  sun, 
falling  on  so  flat  a  surface,  and  being  continually 
reflected  from  the  water,  must  afford  a  great  degree 
of  heat  to  the  air.  At  the  same  time  this  will 
account  for  the  sun^s  being  seen  by  the  Dutch  in 
Nova  Zembla  a  fortnight  earlier  than  he  should  have 
appeared,  according  to  astronomical  calculations.* 
Many  other  circumstances  might  be  mentioned,  but 
these  will  doubtless  occur  to  the  intelligent,  and 
therefore  it  is  unnecessary  to  dwell  longer  upon 
them. 

The  gseat  injustice  of  rejecting  opinions,  on  ac- 
count of  their  appearing,  at  first  sight,  paradoxical, 
or  somewhat  inconsistent  with  notions  commonly 
received,  having  been  ckarly  shown,  and  the  mis- 
chievous consequences  flowing  from  it  by  various 
instances  pointed  out;  the  foundatibn  of  this  con- 
jecture, that  there  may  be  a  passage  near  the  Pole, 
having  been  fairly  stated,  the  popular  objections  to 
it  clearly  removed,  the  general  advantage  that  might 
be  expected  from  thence  placed  in  a  proper  light, 
and  the  consistence  of  all  the  circumstances  relative 
thereto,  with  the  established  course  of  nature,  having 
been  also  rendered  evident;  there  can  be  nothing 

■    -  *  See  Purchas,  vol.  iii.  p.  499,  600. 


^  ^.  ..*-jai*».A  _  .4^  fn.^L 


»-*^'.**iw-r».,^_^v  ^     _.,  .^.,5r^-.v;;uJr 


THE  KORTH  POLE. 


lOT 


ive  been 

showing 

l^ht,  have 

ountable. 

fole,  then 

ormed  to 

the  sun, 

ntinually 

t  degree 

this   will 

Dutch  in 

>uld  have 

ulations.* 

)ned,  but 

^ent,  and 

jer  upon 

8,  on  ac- 
'adoxical, 
!ommonlj 

the  mis- 
^  various 
this  con- 
the  Pole, 
ctions  to 
lat  might 
Jer  light, 

relative 
N  having 

nothing 


more  looked  for  respecting  this  matter  merely  in  the 
light  of  a  philosophical  speculation.  But  if  sujh 
porting  this  had  been  the  only  motive,  these  reflec- 
tions had  not  employed  the  time  of  the  writer,  or 
trespassed  so  long  upon  the  reader's  patience.  What 
then  remains?  To  demonstrate,  that,  as  the  pos- 
•ibility,  practicability,  and  facility,  of  such  an  under- 
taking have  been  insisted  upon,  its  national  utility 
should  be  shown  to  deserve  consideration ;  and  that, 
as  it  is  an  object  of  the  greatest  importance  to  the 
public  welfare,  its  execution  should  be  no  longer 
delayed.  There  is  unquestionably  no  country  in 
Europe  so  well  situated  for  such  an  enterprise  as 
this.  The  transit  from  Shetland  to  the  Northern 
parts  of  Asia  would,  by  this  way,  be  a  voyage  only 
of  a  few  weeks.  The  inhabitants  of  these  islands 
and  of  the  Orkneys  are,  and  have  been  for  many 
yea^,  employed  in  the  Greenland  Fisheries,  and 
the  natives  of  these  isles  are  the  persons  mostly 
sent  to  the  establishments  in  Hudson's  Bay^  By 
these  means  they  are  inured  to  cold,  to  ice,  and 
hard  living,  and  are  consequently  the  fittest  for 
being  employed  in  such  expeditions.  When  thi? 
shall  be  once  executed  with  success,  it  will  necessa- 
rily bring  us  acquainted  with  new  Northern  countries, 
where  ordinary  clothes  and  other  coarse  woollen 
goods  will  probably  be  acceptable,  new  channels  of 
commerce  would  be  thereby  opened,  our  navigation 
extended,  the  number  of  our  seamen  augmented, 
without  exhausting  our  strength  in  settling  colonies, 
exposing  the  lives  of  our  sailors  in  tedious  and  dan- 
gerous voyages  through  unwholesome  climates,  or 


'^ 


•V, 


»t . 


^i 


*  ) 


;-f''' 


V?7 


-5-/\' 


^ 


t 


lOff 


ON  APPROACHING 


^r-VV 


haring  any  other  trade  in  prospect  than  of  exchange 
ing  our  native  commodities  and  manufactures  for 
those  of  other  countries.    This,  if  it  could  be  brought 

'  about,  would,  in  the  first  instance,  convert  a  number 

«  of  bleak  and  barren  islands  into  cultivation,  connect 
them  and  their  inhabitants  intimately  witii  Fritain, 
give  bread  to  many  thousands,  and  by  providing 
suitable  rewards  for  many  different  species  of  indus- 
try, encourage  population,  and    put  an  easy  and 

;  effectual  period  to  the  mischiefs  and  scandal  of 
emigrations.  The  benefits  derived  from  these  dis- 
coveries, and  the  commerce  arising  from  them,  will 
necessarily  extend  to  all  parts  of  our  dominions.  For 
however  fit  the  poor  people  of  those  islands  may  be 
for  such  enterprises,  or  however  commodious  the 
ports  in  their  countries  may  be  found  for  equipping 

-  and  receiving  vessels  employed  in  these  voyages,  yet 
the  commodities,  manufactures,  &c.  must  be  furnished 
from  all  parts  of  the  British  empire,  and  of  course  be 
of  universal  advantage.    These,  as  they  are  true, 

i  Will  it  is  hoped  appear  just  and  <:^ogent  reasons  for 
Wishing,  that  a  project,   which  has  dwelt  in  the 

,,  mouths  and  memories  of  some,  and  in  the  judgment 
and  approbation  of  a  few,  from  the  time  of  Henry 
the  Eighth,  should  be  revived,  and,  at  length,  for 

<  the  benefit  of  his  subjects,  carried  into  effect,  under 
the  auspices  of  George  the  Third, 


,hl^-<»W'^ 

")y^'^ 

•^^•i 

*:^>, 

'1^\ 

■  4^ 

Ah 

\M 

^M 

-   ^"■*, 

_y 

A^-'c  ^  -^ 

^V 

:■%' 

''k-U 

^L;^ 

,      ! 

•• 

■r.' 

-  '>lf^  ';'-»^ 


'>SS 


■*®T 


« 


TBB  NORTH  POLE. 


109 


exchange 
tures  for 
B  brought 
number 
connect 
i  Prituin, 
providing 
of  indus- 
asy  and 
;andat  of 
hese  dis- 
lem,  will 
ons.   For 
8  may  be 
lious  the 
equipping 
^ages,  yet 
furnished 
course  be 
are  true, 
asons  for 
it  in  the 
judgment 
)f  Henry 
ngth,  for 
;t,  under 


»* 


f  have  mentioned  in  the  preceding  sheets,*  that  I 
expected  some  additional  instances  of  Dutch  ships, 
which  had  been  in  high  Northern  latitudes ;  but, 
though  I  delayed  the  publication  for  some  weeks, 
they  did  not  arrive  time  enough  to  appear  with  the 
others.  I  have  however  «ince  received  them 
from  Professor  Allamand  of  Leyden,  F.R.S.,  by 
means  of  Mr.  Valltravers,  F.R.S.,  &c.,  and  take 

'',  the  earliest  opportunity  to  lay  them  before  the 

/  public,  as    a    valuable   addition    to   the   former 

f  papers. 


TO  THE  HONOURABLE  DAINES  BARRINGTON^ 
sw, 

"■i  Having  made  some  inquiries  (agreeable  to  your 
desire)  from  Professor  Allamand,  of  Leyden,  F.R.S. 
with  regard  to  Dutch  Navigators,  who  have  reached 
high  Northern  latitudes;  he  has  been  so  kind  to 
send  me  the  following  account,  drawn  up  by  Captain 
William  May,  a  very  distinguished  and  experienced 
sea-officer  in  the  Dutch  service,  which  begins  with  a 
letter  from  Mr.  John  Walig  to  his  owners,  who  has 
been  master  of  a  Greenland  ship  ever  since  the  year 
1740. 

*  '  I  am,  &c. 

.f  ROD.  VALLTRAVERS.  ? 


-.r-. 


¥ 


*  In  the  additioiwl  papers  frQin  Hull,  p.  6£. 


-i*. 


l«'->^ 


-«e 


# 


•y» 


ttw 


% 


'■•;>. 


siSi 


«<*"■ 


M- 


110 


ON  APPROACHING 


•«  TO  MESS.  NIC.  AND  JACOB  VAN  STAPHORST. 

"fleWer,  Jan.  3,  1775. 

"  In  answer  to  your  letter  of  the  22d  of  Decem- 
ber concerning  the  question,  whether  we  have  been 
nearer  to  ^the  Pole  than  80i%  I  must  inform  you,  that 
^  we  have  been  often  to  81%  near  the  Seven  Isl- 
ands, to  the  Northward  of  the  Northeast  Land,  and 
some  have  been  in  82%  but  then  not  clear  from 
ice,  in  which  they  drove  about.  I  never  heard  of 
any  discoveries  made  there,  as  they  have  always  been 
fishers,  who,  driving  with  the  ice  to  the  Northward, 
lea\Le  that  direction  upon  getting  room ;  and  when 
*  now  and  then  the  sea  has  been  free  from  ice,  that 
has  happened  commonly  in  the  months  of  June  and 
July.  In  1763,  I  spoke  with  a  Scotch  Captain  in 
Greenland,  who  told  roe  he  had  been  to  83%  that  the 
sea  was  then  free  from  ice,  but  that  he  had  made  no 
discoveries,  without  mentioning  any  more  particulars, 
ibr  we  ask  after  nothing  but  whales.  When  I  spoke 
to  him  it  was  in  July,  and  then  we  could  get  no 
farther  North  than  79*  30'  for  the  ice.  In  short,  we 
can  seldom  proceed  much  higher  tht^n  801°,  but 
almost  always  to  that  latitude,  for  it  seems  that  the 
conjunction  of  the  currents  often  fastens  the  ice  there. 
I  fished  last  year  from  80'  25'  to  80°  35',  according  to 
the  land  we  made  afterward. 

"But  in  the  year  1707,  Captain  Cornelius  Gillis, 
having  gone  without  any  ice  far  to  the  Northward  of 
81%  sailed  to  the  North  of  the  Seven  Islands,  pro- 
ceeded from  thence  East,  and  afterward  Southeast, 
iiemaining  to  the  East  of  the  Northeast  Land,  when 


«* 


cominj 
twentj 
east  M 
no  bo 
Spitzl 
ice,  I 
most  < 
in  the 
and  n 


'**<^'-    : 


^^' 


^m 


f^^ 


THE  NORTH  POLE. 


Ill 


RST. 
3,  1775. 

Decem- 
ave  been 
you,  that 
even  Isl- 
and, and 
ear  from 
heard  oi 
mya  been 
)rthward, 
nd  when 
ice,  that 
June  and 
Eiptain  in 
,  that  the 
made  no 
rticulars, 
I  spoke 
1  get  no 
hort,  we 
tor,   but 
that  the 
ce  there. 
»rding  to 

IS  Gillis, 
ward  of 
ds,  pro- 
•utheast, 
1,  when 


coming  again  to  latitude  80°  he  discovered  about 
twenty-five  miles*  East  from  the  country  to  the  North- 
east very  high  lands,  on  which,  as  far  as  we  know, 
no  body  has  ever  been.  As  to  the  season  when  the 
Spitsbergen  seas  may  be  expected  to  be  &ee  from 
ice,  I  believe,  according  to  my  observations,  that  the 
most  open  sea  to  the  Northward  generally  happens 
in  the  month  of  September,  but  then  the  nights  begin, 
and  make  the  navigation  dangerous. 

*^  I  am,  &c.  ^ 


>"■ 


■js-    '    ' 


■>     ■•-■ 


"JOHN  WALIG." 

i,    .  ■  .  J,  • 

♦  Fifteen  to  a  degree,  at  the  Equator. 


ttey  ?■ 


rvv- 


r,"-  ^* 


O.'  '  y  M:>< 


# 


''^WiflBf^ 


■i^ 


5r    ' 


»".■    'i 


¥ 


*^; 


»„J 


^- .  .•/ 


■** 


w- 


■ »  i1 


.# 


..>-' 


^i?"- 


v^' 


,**■" 


.*««iv,:-J..^||fifb,..  .-«<|i»-. 


V,  - 


■"i^ 


■^' 


A  SHORT 


ACC017NT  OF  NAVIGATORS, 


WHO  |UT*  IBACIIBO 


HIGH  KOBTHEBN  LATITUDES.* 


I  WENT  to  Amsterdam  the  26lh  of  March,  beii^g  the 
most  proper  jtime  to  make  the  desired  inquiries,  and  to 
obtain  information  from  all  the  conunand^s  that  weite 
to  depart  this  year  to  Greenland;  for  then  you  meet 
six,  eight,  and  more  together,  in  houses  where  thejf 
enlist  their  men.  I  am,  however,  sorry  to  mention, 
that  but  few  of  those  commanders  keep  joumak 
when  they  are  near,  or  in  the  ice ;  but,  notwithstand- 
ing (his,  the  accounts  they  ^ve  carry  with  them  such 
an  air  of  truth,  from  being  confirmed  by  minute  .cir- 
cumstances, and  corroborated  by  so  many  witnesses, 
that  these  relations  (I  verily  believe)  may  be  de- 
pended upon  as  well  as  some  journals.  I  partica- 
larly  applied  myself,  however,  to  those  to  whcMD  a 
great  number  of  voyages  bad  given  experience,  and 
(contrary  to  my  expectations)  met  with  men  of  can- 

*  TKhi  account  was  drawn  qp  by  Captain  William  May,  in  the 
service  of  the  States,  at  the  desire  of  Professor  Allamand  of  Leyden. 
—See  p.  7^. 

IS 


^' 


■A 


% 


■m. 


IN 


UN   APFKOACIIIMI 


dour  and  penetration.  I  tliought  it  proper  likewise, 
to  take  the  following  extract  of  a  Journal,  it  showing 
the  common  form  in  which  some  of  them  are  kept. 


* 


$ 


i 


% 


Tratulation  of  a  part  of  a  Jonrnal,  kept  on  hoard  the  Vrom  Maria, 
Om/mandtr  Martin  Breet. 

N.  B.  The  sun^s  altitudes  were  taken  with  an  octant, 
and  twelve  minutes  allowed  for  the  sun^s  semi- 

^  diameter,  refraction,  and  dip  of  the  horizon ;  the 
longitude  from  Tenerifie;  the  miles  fifteen  to  a 
degree  at  the  Equator;  the  bearings  with  a  com- 

^    pass  unrectified.  „ 

The  22d  of  April,  1771,  sailed  from  the  Texel  for 
Greenland.  8th  of  May,  latitude,  according  to  the 
run,  7(f  33*,  longitude  l^  22';  saw  the  first  ice.        ^ 

13th  ditto,  latitude  74**  50*,  longitude  24"  35';  met 
with  a  border  of  ice. 

14th  ditto,  latitude  by  observation  75**  44',  longi- 
tude 26**  13';  came  against  some  ice. 

15th  ditto,  latitude  76"  13',  longitude  25**  40';  saw 
Spitzbergen,  the  South  Cape;  bore  East  Northeast 
fourteen  miles. 
N.  B.    Drove  about  in  the  ice ;  made  fast  to  a  field. 

25th  ditto,  in  the  morning  saw  the  North  F(Hreland. 
Northeast  by  East,  latitude  79**  12*,  longitude  20**  40^. 

26th  ditto,  longitude  by  observation  79**  10'. 

27th  ditto,  against  the  ice. 
<    28th  ditto,  passed  through  some  ice. 

29th  ditto,  got  fast  in  the  ice;  saw  two  ships  sail 
ihg  pretty  freely  in  the  East  Northeast.  4^,  1 

N.  B.  In  the  ice  till  the  *^  r  w  ' 


XV 


•ia>afi6i«a'iM' 


n 

^^.* 


THE  NORTH  POLE. 


115 


ikewise, 
showing 
kept. 

'ow  Maria, 


n  octant, 
1*8  semi- 
zon;  the 
een  to  a 
h  a  com- 

'cxel  for 
ng  to  the; 
ice. 
35';  met 

14',  longi- 

40';  saw 
Northeast 

to  a  field. 
Foreland. 
le  20'  4(y. 
10'. 

jhips  sail- 


7th  of  June^  got  more  room  t  beat  to  the  Southward, 
and  made  fast  to  a  field ;  saw  land  in  the  East  North- 
east, distance  fourteen  or  fifteen  miles ;  supposed  it 
the  Quade  Hoek,  latitude  by  observation  79°  58^; 
made  fast  to  the  ice  till  the 

11th  June,  at  noon;  a  violent  storm,  wind  South- 
west, latitude  by  observation  80"  19'.    In  the  night, 
drove  towards  the  coasts,  for  it  blew  too  hard  to  carry  < 
sail. 

12th  ditto,  in  the  morning,  laid  fast  in  the  ice* 
the  storm  continued,  and  the  ship  so  much  pressed 
by  the  ice,  that  we  were  obliged  to  unhang  the 
rudder. 

•  13th  ditto,  hard  pressed  by  the  ice,  latitude  by 
observation  80**  29*.  Remained  pressed  by  the  ice 
UUthe 

18tb  ditto,  latitude  by  observation  80^  50^;  the  ship 
not  moveable. 

19th  ditto,  latitude  by  observation  80**  57';  the  ice 
in  great  motion. 

20th  ditto,  fast  in  the  ice  again,  latitude  by 
observation  80*^  dS*;  calm  till  the 

24di  ditto,  began  to  blow  a  storm ;  got  some  room 
in  the  ice. 

'.   25th  ditto,  having  got  more  room  we  advtoced. 
.    26th  ditto,  locked  up  again. 

27th  ditto,  saw  the  land,  namely,  the  Dorro  Hoek, 
South  by  East  half  East,  and  the  Vlakke  Hoek,  East 
Southeast ;  lay  beset  till  the 

29th  ditto,  latitude  by  observation  80°  16'. 

30th  ditto,  wind  Northeast. 


■T. 


*. 


■•.-iM&A, 


'Vttr'- 


n'tfSMp^^'^^  . 


'«. 


116 


ON  APPROACHING 


?1.'- 


f  1st  of  July,  8KW  t^ater  in  the  West  Southwest, 
which  we  had  not  seen  for  many  days.  In  the  after- 
noon got  iBore  room. 

2d  ditto,  worked  our  way  through  as  much  ice  as 
we  could,  wind  East  Northeast,^  towards  the  evening 
North ;  made  fiust  to  a  field. 

.3d  ditto,  at  noon,  saw  the  land,  being  the  Robbe 
Bay,  bearing  Southwest  by  West  about  one  mile. 


I  have  left  out  many  little  circumstances  respecting 
the  wind,  tides,  &c.,  as  thinking  the  above  sufficient  for 
ascertaining  the  latitudes,  and  to  show  the  method  in 
which  many  of  the  Greenland  Masters  keep  their 
Journals.  That  year  seems  to  have  been  favourable 
finr  gettii^  more  to  the  North;  for,  notwithstanding 
Mr.  Breet  met  with  so  much  ice,  from  the  latitude  of 
79"*  30'  to  that  of  80''  58',  Captain  Jan  Klaas  Castri- 
cum,  in  the  ship  the  Jonge  Jan,  at  that  very  time  of 
the  year,  and  nearly  in  the  same  longitude,  resMshed 
81**  40',  by  the  medium  of  several  observations  with 
forestafis,  where  he  fished  with  success,  in  company 
with  Witje  Jelles,  who  sailed  fi'om  Hamburgh,  and 
found  but  little  ice.  There  were  likewise  two 
English  ships,  who  sailed  so  far  to  the  North,  that 
Castricum  lost  sight  of  them  from  the  mast  head, 
which  two  ships  returned  in  something  more  than  two 
days,  and  the  Captains  came  on  board  of  Castricum,* 
and  assured  him,  that  they  had  been  to  upwards  of 


"d"--^"H* 


*  Captain  Castricum  neither  asked  their  names,  nor  those  of  their 
aliips ;  all  that  he  knew  was,  he  said,  if  he  remembered  right,  they 
sailed  from  England* 


■  ^'.. 


'^% 


-m^ 


iif^> 


'« 


y^iFli'-v  -.^^llWl^Oi 


«f" 


louthwcBt, 
the  after- 

ichice  as 
e  evening 

he  Robbe 
i  mila  ' 

respecting 
ifficient  for 
method  in 
keep  their 
favourable 
ithstanding 
latitude  of 
aas  Castri- 
srytime  of 
e,  reached 
ations  with 
n  company 
burgh,  and 
:ewise  two 
N[orth,  that 
oiast  head, 
re  than  two 
!^astricum,* 
upwards  <rf 

r  those  of  their 
red  right,  they 


W 


THE  NORTH  POLE. 


Ill 


&3%  and  rould  have  gone  much  farther,  as  they  had 
no  obstructions  from  ice,  but  finding  no  whales  thej 
returned.  I  spoke  at  the  same  time  with  other  cpm- 
manders,  who,  having, been  in  sight  of  those  ships, 
confirmed  Castricum^s  account. 

Six  of  the  oldest  Masters  assured  me  (amongst 
whom  were  John  Walig,  Klaas  Keuken,  and  J.  Klaaa 
Castricum,)  that  they  had  known,  firom  1730  to  1742, 
an  old  English  commander,  whose  name  was  Krick- 
rack  ;*  it  was  his  custom  between  the  fisheries,  if  not 
obstructed  by  ice,  to  sail  to  the  Northward;  and 
some  of  them  affirm,  that  when  they  have  been  at  an 
anchor  in  Brandewyns  Bay,  he  once  stayed  away 
ten,  and  at  another  time  twenty  days,  before  his  re- 
turn, and  they  are  very  sure  that  he  reported  (and 
they  have  reasons  to  believe  him)  that  he  had  been 
two  degrees,  and  even  more,  North  of  the  Sevei> 
Islands.  All  I  could  farther  learn  of  this  Mr.  Krick- 
n|ck  was,  that  in  1740  he  was  in  the  only  diip  sent 
from  England ;  that  for  several  voyages  he  had  the 
same  ship^s  company ;  that  in  or  about  1742  he  had 
the  command  of  a  transport,  on  board  of  which  he 
lost  his  life  by  a  musket  ball :  they  were  certfiin  that, 
he  kept  Journals,  out  of  which  they  think  much  light 
might  be  obtained.  ' 

The  greatest  part  of  the  Dutch  commanders  live 
at  the  Helder.  Mr.  Walig  and  others  assured  me, 
that  the  most  Northern  voyage  then  ever  heard  of, 
and  on  which  they  could  with  certainty  depend,  was 

*  From  1736  to  1740,  most  of  the  Masters  of  Eng^sh  Ships,  fitted 
out  for  the  Greenland  Trade,  were  Dutchmen. 


% 


. 


*fm: 


fV      -; 


i  1 

i 


.m»'-  "  a*<WSi<<«Himir>  t 


* 


1X8 


ON  AFFROACHING 


I 


^ 


:*' 


that  of  Jacob  Scliol  in  1700,  who  had  been  so  far 
North,  that  on  his  return  he  sailed  with  a  fresh  gale 
of  wind,  due  South,  forty-eight  hours,  and  then  fell 
in  with  the  Seven  Islands ;  he  consequently  had  been 
(reckoning  that  run  at  only  four  Dutch  miles  an  hour, 
which  they  thought  too  little)  in  upwards  of  84^  North 
latitude.  As  Mr.  Schol  was  an  inhabitant  of  the  Hel- 
der,  they  told  me  that  they  would  strive  to  procure 
me  his  papers  from  his  heira ;  and,  if  I  mistake  not, 
they  said  that  they  had  actually  seen  those  papers 
in  their  younger  days. 

Finding  that  Mr.  Van  Keulen  had  put  down  (in  his 
chart)  the  land  discovered  by  Captain  Gillis,  men- 
tioned in  Mr.  Walig^s  letter,  I  went  to  him,  to  see  on 
what  foundation  he  had  placed  that  discovery;  but 
as  those  papers  could  not  be  found,  I  applied  to  Mr;^ 
Walig,  who  told  me,  that  Mr.  Cornelius  Gillis  had 
"been  an  inhabitant  of  the  Helder;  that  Walig, 
together  with  Mr.  Keuken^  Mr.  Baske,  and  others^: 
since  dead,  had  often  examined  Gillis^s  papers,  maps, 
&c.,  and  found  that  he  was  an  enterprising  man,  and 
very  accurate  in  his  remarks  and  charts ;  that  his 
grahds(m  had  his  Journals  and  other  Papers  in  his 
possession;  and  his  granddaughter,  who  was  mar- 
ried to  an  officer  of  Walig's  ship  (who  had  formerly 
been  a  conmiander)  had  his  charts,  some  of  which 
that  officer  generally  took  with  him,  in  order  to  cor- 
rect them.  I  begged  hard  to  have  them,  if  only  for 
twenty-four  hours ;  and  next  morning  Mr.  Walig  put 
into  my  hands  the  original  draughts  of  all  the  dis- 
coveries Mr.  Gillis  ever  made  with  regard  to  Spitz- 
bergen,  excepting  some  particular  drawings  of  bays 


•«■'•■■ 


,...  .,^fi 


•4 


-^^. 


^ 


it^-    THE  NORTH  POLK. 


119 


en  so  iar 
esh  gale 
then  fell 
lad  been 
an  hour, 
4'  North 
the  Hel- 
procure 
itake  not, 
e  papers 

vn  (in  his 
lis,  men- 
to  see  on 
^ery;  but 
ed  to  Mr. 
iriUis  had 
It  Walig, 
id  others, 
;rs,  maps, 
man,  and 
;  that  his 
irs  in  his 
was  mar- 
L  formerly 
of  which 
?r  to  cor- 
r  only  for 
kValig  put 
11  the  dis- 
to  Spitz- 
s  of  bays 


and  views  of  land,  with  permission  to  keep  them  in 
my  possession  tiU.  Mr.  Walig's  return  from  Green- 
land ;  copies  of  which  are  here  annexed,*  and  Mr. 
Walig  promised  to  procure  me,  if  possible,  all  the 
papers  of  that  old  commander,  before  he  left  the 
Tei^el,  which  I  hope  to  receive  in  a  few  days,  and 
shall  not  fail  in  sending  over  every  thing  I  find  mate- 
rial. Asking  what  particulars  Mr.  Walig  and  others 
remembered  out  of  those  papers,  they  gave  the  fol- 
lowing account,  That  Mr.  Gillis  passed  more  than  a 
degree  to  the  Northward  of  the  Seven  Islands,  with- 
out any  hinderance  from  ice ;  that  he  proceeded  East 
for  some  leagues  with  an  open  sea,  then  bent  his 
course  Southeast,  and  afterward  South ;  saw  in  the 
latitude  of  80%  to  the  East,  very  high  land;  run 
through  the  East  coast  of  the  Northeast  land,  and 
entered  the  Waygat  Straits.;  vcame  to  an  anchor  in 
Lamber  Bay,  and  took  two  whales,  and  from  thence 
j>roceeded , to  the  Texel.  Mr.  Baske  gave  .also  an 
account  of  his  uncle's  having,  in  company  with  three 
ships,  entered  Waygats  from  the  North,  and  advanced 
as  far  as  the  same  bay,  but  found  too  much  ice  to  get 
through,  of  which  the  other  three,  being  young  com- 
manders, made  a  trial.  The  North  passage,  how- 
ever, on  their  return  being  shut,  and  it  being  the 
beginning  of  September,  they  made  preparation  to 
leave  their  ships,  in  order  to  get  over  land  to  Smee- 
renberg,  but  the  ice  luckily  giving  way,  they  got  out 
to  the  Northward.    Mr.  Baske,  who  is  a  curious  man^ 


*  These  were  copies  of  the  draughts  of  the  different  coasts  of 
Spitzberg«in,  of  which  Captain  Gillia  hath  taken  accurate  surveys. 


i 


lit 
% 


% 


4' 


^% 


# 


% 


m*^*' 


120 


ON  APPROACHING 


■{■■'i 


f 


':  \ 


~1K* 


pronused  me,  amongst  other  things,  his  tihennome' 
trical  observations,  which,  by  the  conversation  I 
had  abont  them,  I  have  reason  to  think  will  be 
accurate. 

After  having  passed  six  mornings  with  a  great 
number  of  our  commanders  quartered  in  diii^nt 
houses,  i  find,  Chat  scarcely  a  year  bad  passed  but 
Bome  tX  them  have  been  to  81°  North,  but  rarely 
£)und  the  seas  free  firom  ice. 

This  is  all  the  infonnatito  I  have  been  able  to  pro- 
cure during  my  short  stay  at  Amsterdam,  which 'I 
would  have  prolonged,  if  a  call  to  the  Hague  had 
not  prevented  me.  I  can  onlyadd,  that  waiting  upon 
Mr.  Boreel,  that  gentleman  promised  that  he  would 
order  a  search  to  be  made  for  the  Joumsds  of  those 
shipS:,  which  were  formerly  employed  in  protecting 
our  Greenland  fisheries.  '  s^.m. 
w\  must,  however,  not  forget  to  mention  a  particular 
&at  Mr.  Van  Keulen  acquainted  me  with.  He  had, 
lat  his  house  last  summer,  a  conversation  with  a  Rus- 
sian, who  had  passed  the  winter  last  year  in  Spitz- 
bergen,  and  gave  lum  the  following  account.  That 
being  in  the  utmost  distress,  for  want  of  eatables,  on 
the  North  coasts  he  made  a  trial  to  get  with  his  boat 
tawards  the  middle  of  the  island,  by  means  of  the 
Bay  of  Wyde  Bay  in  Gillis's  map,  into  which  he  pro- 
ceeded, till  to  his  great  surprise,  he  fell  into  V^ }  ;>e 
Jansz^s  Bay,  and  so  came  out  to  the  South  of  Spitz- 
bergen ;  but  he  bad  taken  no  notice  of  the  depths  of 
water.  Being  questioned  as  to  that  particular,  he 
«aid  he  was  very  sure  that  he  did  not  pass  through 
theWaygats. 


* 


^ 


•TVf  '^ 


#, 


„..a 


jf^* 


V.4  -  ••-J- 


"ftS 


vermome' 

creation  I 

will  be 

a  great 

different 

assed  but 

)ut  rsurely 

t 

)le  to  pro- 
which'I 
ague  had 
iti^tipon 
he  would 
8  of  those 
protecting 

particular 
He  had, 
(ith  a  Rus- 
r  in  Spitz- 
int.  That 
itables,  on 
th  his  boat 
a,ns  of  the 
ch  he  pro- 
into  W}  je 
t  of  Spitz- 
;  depths  of 
ticular,  he 
iss  through 


«:. 


iM*<^«  ■-.•,j' 


jp»  '^ 


THE  NORTH  POLE. 


121 


In  all  my  conversations  with  our  Greenland  cosor 
manders,  I  never  failed  to  ask  which  course  they 
would  take  to  reach  high  Northern  latitudes;  the 
result  was,  that  they  would  never  seeL  it  to  the 
Westward  of  Spitzbergen,  but  run  out  to  the  North, 
from  the  West  coast  of  Nova  Zembla ;  Mr.  Baskets 
reasons  and  those  of  other  commanders  were, 
1st,  That  all  the  Western  coasts  of  the  Northern 

countries  were,  for  the  most  part,  free  from  ice, 

occasioned  by  the  winds  and  tides  chiefly  coming 

from  the  East,  which  experience  proves. 
2d,  That  the  ice  comes  originally  from  the  Tartarian 

rivers  j  for,  that  the  sea  never  freezes  but  where  it 

is  calm,  and  at  the  same  time  a  great  quantity  of 

snow  falls. 
3d,   That  near  the  Seven  Island,  navigators  often 

meet  with  a  great  Northeast  Swell,  which  proves, 

that  at  such  time  the  sea,  to  a  considerable  distance 

to  the  Northeast,  is  not  locked  up  by  the  ice. 
4th,   That  the  drift  wood  could  not  come  to  the 

Northward  of  Spitzbergen,  in  case  the  seas  be*- 
'  tween  the  North  of  Asia  and  that  island  were  fi*o- ' 

zen;   whereas  a  great  quantity  of  that  wood  is 
'driven  on  the  North  coast  of  Iceland,  which  is  a 

demonstration  that  the  currents  come  from  the 

Northeast. 
5th,  That  in  some  of  the  trees  the  marks  of  the  axe 

were  very  plain,  and  the  colour  of  the  wood  so  ' 
r  fresh,  that  they  certainly  had  not  been  six  months 

in  the  sea. 
dih.  That  some  whole  trees  appeared  with  buds 

thereon,  which  they  think  could  not  have  remained 

16 


■flW 


*^ 


"'^m 


m: 


•■"■■  ■!■>»»'«!/ 


^' 


122 


ON  APPROACHING 


'¥J(! 


'•!»■■ 


(>'  80  fresh,  if  the  trees  had  been  a  year  in  the  salt 

'^-  'water.  'f 

7thv  That  the  East  of  Greenland  was  now  discovered 

"'  to  the  latitude  of  791',  that  it  probably  extended 

'  farther  to  the  North  Northeast,  which  they  look 

upon  to  be  the  cause  of  the  stoppage  of  ice  be- 

tween  that  coast  and  Spitzbergen,  and  the  reason 

'     why  they  never  find  a  Northwest  or  Northerly 

swell. 
8th,  That  generally  all  ships,  which  had  once  got  to 
the  North  as  far  as  82°,  met  with  little  or  no 
obstructions  firom  the  ice ;  and  more  arguments  to 
the  same  purpose.    There  were  some,  however, 
would  rather  make  the  trial  between  Spitzbergen 
and  the  land  discovered  by  Mr.  Gillis. 
N.  B.    They  knew  nothing  of  the  Papers  read  before 
Hhe  Royal  Society. 


.  -W: 


TO  ROD.  VALLTRAVERS,  ESQ.  tic. 


SIR, 


Professor  Allamand,  being  very  desirous 
that  the  inclosed  might  be  sent  to  you  as  soon  as  pos- 
sible, has  obliged  me  to  draw  up  with  haste  the  above 
account  of  Hie  informations  I  received  at  Amsterdam. 
In  reading  it  over  and  comparinj^  it  with  my  notes,  I 
find  no  fault  as  to  the  facts  rela-ed,  vrhatever  there 
maybe  in  the  manner  in  which  it  is  drawn  up ;  in 
case  the  whole  or  any  part  of  it  should  be  thought 
worth  publishing,  I  hope  you  will  be  bo,  good  as  to 
have  it  corrected.* 

*  This  hath  been  done  in  some  trifling  particulars,  relatire 
merely  to  the  style,  as  Captain  May  is  not  a  native  of  England. 


■(»..»» 


..r' 


# 


^ 


*r  ft 


iSt 

• 

1^ 

THE  NORTH  rOLE. 

123 

I  could  have  made  it  more  circumstantial,  as  my 
notes  are  very  full,  in  particular  with  regard  to  the 
reasons  our  commanders  gave  for  not  making  the 
trial  to  the  West  of  Spitzhergen,  &c. 

I  am  informed,  that  Mr.  De  Bougainville  intends 
to  go  by  the  way  of  Nova  Zembla* 
I  am,  with  profound  respect. 

Sir,  , 

^  Your  most  obedient  humble  Servant,  i^ 

WILLIAM  MAY. 
Leydtn,  April  nth,  mb. 


m 


'•yH*» 


'■■■ir  ■ 


.a* 


Thus  do  the  Dutch  seamen,  employed  in  the 
Greenland  fishery,  agree  with  our  own  countrymen, 
in  never  having  so  much  as  heard  of  a  perpetual  bar- 
rier of  fixed  ice,  to  the  Northward  of  Spitzhergen,  in 
80T°,t  which  indeed  is  one  of  their  most  common 
latitudes  for  catching  whales,  whilst  all  of  them  sup- 
pose the  sea  to  be  generally  open  in  those  parts,  and 
many  of  them  proceed  several  degrees  beyond  it. 

I  shall  only  add*  that,  in  my  former  pamphlet4  I 
have  mentioned  a  fact  or  two  I  had  reason  to  expect 
from  the  Rev.  Mr.  Tooke,  Chaplain  to  the  factory  at 
Petersburgh,  which  he  conceived  would  strongly 
prove  that  the  sea  is  open  to  the  Pole,  and  which  I 

*  This  voyage  of  discovery,  however,  did  not  take  place,  ^j, 

t  One  of  them  indeed  says,  that  the  ice  frequently  packs  in  that 
'.  latitude,  which  he  supposes  to  arise  from  the  meeting  of  two 
cnrrents. 

4^  Page  47,  note. 


-r^ 


f' 


* 


•# 


'i^- 


m 


•IM'^i-' 


1^ 

124 


■% 
•» 


>v. 


^■■'%'   4' 


ON  APPROACHING 


have  since  received  in  a  letter'from  him  dated  the 
26th  of  May  last. 

Mr.  Tooke  hath  been  assured  by  several  persons, 
who  have  passed  the  winter  at  Kola  in  Lapland,  that 
in  the  severest  weather,  whenever  a  Northerly  w»nd 
blows,  the  cold  diminishes  instantly,  and  that,  if  it 
continues,  it  always  brings  on  a  thaw  as  long  as  it 
lasts. 

He  hath  also  been  informed  by  the  same  authority, 
that  the  seamen,  who  go  out  from  Kola  upon  the 
whale  and  morse  fisheries  early  in  March  (for  the  sea 
never  freezes  there,)  throw  off  their  winter  garments 
as  soon  as  they  are  from  fifty  to  one  hundred  wersts* 
from  land,  and  continue  without  them  all  the  time 
they  are  upon  the  fishery,  during  which  they  expe- 
rience no  inconvenience  from  the  cold,  but  that,  on 
their  return  (at  the  end  of  May,)  as  they  approach 
land,  the  cold  increases  to  such  a  severity,  that  they 
sulier  greatly  from  it. 

This  account  agrees  with  that  of  Barentz,  whilst 

he  wintered  in  Nova  Zembla,t  and  of  the  Russians  in 

Maloy  Brun ;  the  North  wind  cannot  therefore,  during 

the  coldest  seasons  of  the  year^  be  supposed  to  blow 

'  over  ten  degrees  of  ice. 

Governor  Ellis  indeed,  whose  zeal  in  prosecuting 
the  attempt  of  discovering  the  Northwest  passage 
through  Hudson's  Bay  is  so  well  known,  hath  sug- 
gested to  me  an  argument,  which  seems  to  prove  the 


<r-, 


*  Three  wersts  make  two  miles, 
t  See  Thoughts  on  the  Probability,  &c.,  of  reaching  the  North 


Polei 


;::)u^ 


»u)ptv 


^■■4- 


..T 


■  ■«:';■';" 


"ij^d'*?,* 


# 


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■■■•"^  .-r"»iw-./^  .„  .,  ^..., 


.,-*«.:■'  ^^mi^  -.■'•»,t*^'^i)^f/^.*r 


THE  NORTH  POLE* 


11'. 


125 


absolute  impossibility  of  a  perpetual  barrier  of  ice 
from  80i°  to  the  Pole. 

If  such  a  tract  hath  existed  for  centuries,  the 
increase,  in  point  of  height,  must  be  amazing  in  a 
course  of  years,  by  the  snow,  which  falls  during  the 
winter,  being  changed  into  ice,  and  which  must  have 
formed  consequently  a  mountain  perhaps  equal  to  the 
Peak  of  Teneriffe.*  Now  the  ice  which  sometimes 
packs  to  the  Northward  of  Spitzbergen,  is  said  com- 
monly not  to  exceed  two  yards  in  height. 

D.  B .  \ 

*  Mr.  De  Luc  observes  also,  that  the  ice  upon  the  Glaciers  ia 
always  increasing. — See  his  interesting  observations  on  those  moon- 
tains  of  Switzerland.  A,.  ..,„ 


1 


( 1 


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\*' ■.•  •'' -"^"  '    <t' 


y. 

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*.*  .- 

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Ife 


« 


•> 


»* 


OBSERVATIONS 


^.  ^ 


v.v- 


'(^ 


■^^m-  '^ 


on  THI 


FLOATING  ICE, 

WBIOH  II  rouND  itr 

I     HIGH  NORTHERN  AND  SOUTHERN  LATITUDES. 

SiNCF  the  return  of  the  King's  ships  from  voyages 
of  discovery,  both  in  high  Northern  and  Southern  lati- 
tudes, I  have  found  that  it  hath  been  a  disputed  point, 
whether  the  ice  which  they  have  met  with  was  formed 
chiefly  from  the  salt  or  fresh  water.  I  should  rather 
conceive  that  this  doubt  must  have  arisen  from  what 
is  mentioned  by  the  great  Mr.  Boyle,  in  his  experi- 
ments on  heat  and  cold ;  or  from  an  observation  of 
M.  Adanson,  at  the  end  of  his  voyage  from  Senegal, 
because  from  the  quantity  of  ice  merely  (at  least  to 
the  Northward)  the  early  navigators  never  conceived 
that  it  was  produced  from  sea  water. 

In  full  proof  of  this,  not  to  state  the  opinion  of 
several  others  on  the  same  head,  I  shall  content 
myself  with  citing  that  of  Sir  Martin  Frobisher,  who 
is  well  known  to  have  made  three  successive  voyages 
to  Greenland,  with  a  farther  intent  of  discovering  the 
Northwest  passage  firQm  Europe  to  the  Pacific  ocean. 


'■-V 


S  '^ 


m 


I 


/ 


:'>< 


128 


f 


ON  APPROACHING 


f^^ 


K 

i 

r 


j»^ 


III  the  second  voyage  of  this  celebrated  navigator, 
he  observes : — 

**  We  found  none  of  these  islands  of  ice  salt  in 

taste,  vt'hereby  it  appears  that  they  were  not  of  the 

jf       ocean  water  congealed,  which  is  always  salt,  but  of 

some  standing  or  little  moving  lakes ;  the  main  sea 

freezes  not,  and  therefore  there  is  no  Mare  Glaciale.'''' 

In  his  third  voyage  he  most  anxiously  repeats  this 
same  opinion,  and  in  still  stronger  terms,  so  that 
what  he  hath  thus  laid  down  was  not  an  occasional 
observation  merely,  but  what  he  had  mpch  reflected 
upon,  and  found  to  be  confirmed  by  his  experience 
in  those  Northern  seas.* 

This  opinion  of  Sir  Martin  Frobisher's  seems  not 
io  have  been  disputed  by  any  one,  till  the  time  of 
Mr.  Boyle,  who  observes,  that  there  are  several  in 
Amsterdam,  who  used  to  thaw  the  ice  of  sea  water 
for  brewing,  and  then  cites  Bartholinus  De  jyivis  usu. 
it  De  ghcie  ex  aqud  marind,  certum  est  si  resolvatur^  sal- 
sum  saporem  deposuisse^  quod  non  ita  pridem  experius  est 
Clarissimus  Finkius  in  glaciei  frustisy  ex  portu  nostro 
dlaiis^'\  ■  .♦^  ''  A.  ^ 

I  shall  not  now  criticise  either  what  falls  from  Mr. 
Boyle  himself,  or  from  Bartholinus,  though  it  is  very 
clear  that  the  ice  alluded  to  by  both  must  have  pro- 
bably been  formed  from  fresh  water,  either  in  the 
rivers  or  lakes,  which  empty  themselves  into  the  Zuy- 

>  »  See  Hakluyt,  vol.  ii.  p.  G2  and  67.     In  1776,  Mr.  Marshall, 

Captain  of  a  Greenland  ship,  was  so  good  as  to  bring  me  a  bottle  of 
water,  which  was  melted  from  ice  found  floating  in  the  Spitzbergeii 
seas,  and  which  had  not  the  least  saline  taste. 
.<•«  >  V  "       t  Boyle'a  Worl^f ,  vol.  ii.  p.  264.  folio.  ,. 


A 

■^4, 


#:. 


■•^''-   ^^•■■v 


■'■♦ 


•r 


gff^yjg^ 


THG  NORTH  POLL 


139 


der  Sea,  because  I  shall  hereafter  contradict  the 
assertion  of  Bartholinus,  by  the  actual  eiperiuient, 
which  I  have  tried  myself  during  the  late  hard  frost. 

To  do  justice  indeed  to  Mr.  Boyle*  he  afterward, 
upon  more  mature  consideration,  shows  it  to  be  hit 
opinion,  agreeable  to  that  of  Sir  Martin  Frobisher, 
that  the  fresh  water  obtained  from  ice  floating  in  the 
sea  proves  it  could  not  have  been  formed  from  the 
ocean,  **  because  the  main  sea  is  seldom  or  ever 
frozen."* 

The  next  author  who  supposes  that  congealed  sea 
water  is  by  this  process  rendered  sweet  to  the  taste, 
is  M.  Adanson,  who  informs  us,  that,  upon  his  return 
from  Senegal  in  1748,  he  carried  two  bottles  of  sea 
water,  taken  up  on  the  coast  of  Africa,  from  ^est  to 
Paris,  which,  during  an  intense  frost,  was  so  frozen 
as  to  burst  the  bottles,  and  the  contents  afterward 
became  palatable.t 

To  this  fact  I  shortly  answer,  either  that  the  bot- 
tles were  changed,  or  otherwise  that  M.  Adanson 
does  not  meo^MM  the  circumstance  by  which  the  taste 
of  the  sea  v  Miar  was  thus  altered  upon  its  being  dis^ 
solved.  Mr.  Nairne  hath  been  much  more  accurate 
in  stating  his  experiments  with  regard  to  the  freezing 
sea  water,  in  a  paper  read  before  the  Royal  Society 
on  the  2d  of  February,  1776,  as  he  mentions,  that, 
in  order  to  clear  the  ice  from  any  brine  which  might 
adhere  to  it,  he  washed  it  in  a  pale  of  pump  water  for 
a  quarter  of  an  hour,  after  which  he  informs  the 


-■^ir' 


=  -  v«  •. -ti/ 


*  Boyle's  Works,  vol.  ii.  p.  302. 
t  Voyage  an  Senegal,  p.  190. 
—       17 


,  -.'■■•M 


7.  > 


V  T 


'^. 


m 

--N': 


130 


OiN  APPROACHING 


\\ 


Mil 


*■.#' 


.^lisi. 


*      Society,  that  to  his  palate  it  was  perfectlj  free  from 
any  taste  of  salt.  ' 

This  is  most  undoubtedly  the  fact,  but  Mr.  Naime 
does  not  seem  to  be  aware  from  what  circumstance 
the  Ice  thus  melted  had  become  fresh  water;*  and 
indeed  I  must  admit,  that  upon  the  first  experiment 
which  1  made  with  regard  to  freezing  sea  water,  I 
deduced  the  same  inference  that  he  hath  done,  having 
washed  it  in  fr'esh  water  for  the  same  reason  that  he 
did,  viz.  to  get  rid  of  the  brine  which  might  adhere 
to  the  surface  of  the  ice. 

To  determine,  therefore,  whence  this  freshness  in 
the  thawed  ice  might  arise,  I  placed  a  large  piece  of 
what  remained  frozen  (without  being  washed  at  all 


■;_^.y'. 


f^-'^i 


m-i'^'- 


*  As  Mr.  Nairne,  in  his  letter  to  Sir  John  Pringle,  says,  that  one 
of  his  great  reasons  for  trying  these  «xperinient8  was  to  determine 
whether  the  ice,  which  floats  in  the  Northern  seas,  is  formed  from 
the  salt  water  or  not,  he  therefore  should  have  thawed  the  ice  pre- 
cisely under  the  same  circumstances  with  the  sea  water  adhering,  as^ 
the  navigators  take  it  up.     The  truth  is,  that,  if  the  piece  of  ice 

,  formed  from  sea  water  is  at  all  large,  the  adhering  salt  water  can 
scarcely  effect  the  taste  at  all ;  and  I  have  melted  the  central  parts 
of  a  pretty  large  mass,  which  became  very  salt  after  dissolution, 
though  entirely  detached  from  the  sea  water  in  which  it  had  been 
frozen.  "In  the  severe  frost  last  January  (viz.  1775,)  some  salt 
water,  being  set  abroad,  froze  into  an  ice,  which  was  not  solid  but 
porous,  the  hollows  being  filled  with  the  saltest  part  of  the  water, 
for  the  ice  when  drained  was  quite  fresh.    The  salt  water  being  again 

<  set  abroad,  froze  as  before,  what  remained  still  unfrozen  was  now 
become  exceeding  salt,  but  the  ice  drained  and  dissolved  was  little 
if  at  sil  brackish  ;  by  this  experiment,  if  another  time  more  fuUy 
repeated,  it  may  be  found  to  what  degree  the  saltness  of  water  ma}' 
be  increased,  by  continuing  to  freeze  away  the  fresh  water." — Mr. 

,  Barker  in  Phil.  Trans,  vol.  Ixvi.  p.  ii.  1776.  p.  373. 


V 


*%*■ 


\ .  .* . . 


••:»' 


■m 


'^: 


*     ■:,■•" 


*^^ 


.«a 


THE  NORTH  POLE. 


■V  !'-"lf 


131 


in  pump  water)  to  be  dissolved  before  the  fire,  which 
tasted  very  salt,  as  one  might  naturally  suppose. 

The  weather  continuing  to  be  very  severe,  I  froze 
more  sesC  water,  repeating  the  experiment  of  freshen- 
ing it  or  not,  by  leaving  or  not  leaving  it  in  pump 
water,  which  always  turned  out  uniformly  to  be  the 
same ;  and  the  reason  of  which  is  the  following : — 

When  sea  water  is  frozen,  it  does  not  form  ice 
similar  to  that  from  fresh  water,  being  by  no  meant 
BO  solid  or  trcmsparent,  as  it  consists  of  thin  laminae 
or  plates,  between  which  the  brine  is  deposited,  and 
if  the  ice  is  accurately  examined,  the  small  portions 
of  brine  between  the  plates  may  be  easily  distin- 
fished.  If  this  brine  therefore  is  removed,  the 
laminee  of  ice  when  dissolved,  becomes  sweet  to  the 
taste,  but,  if  thawed  together,  with  the  brine  inter'- 
cepted  between  the  laminae,  the  taste  is  salt,  nor  can 
the  ice  be  considerably  divested  of  the  brine,  by 
merely  leaving  it  to  drain. 

Having  satisfied  myself  thus  far  from  the  fireezing 
sea  water  by  the  natural  cold,  and  under  the  com- 
mon circumstances  of  exposing  it  to  the  air  in  small 
china  cups,  I  applied  to  Dr.  Higgins  to  prosecute 
these  trials  with  his  more  ample  apparatus,  and 
knowledge  of  chymistry ;  who  was  immediately  so 
good  as  to  suggest  and  try  the  following  experiments, 
which  will  throw  farther  light  upon  this  subject.* 

'*  It  would  be  great  injustice  to  Mr.  Lomonosoff,  a  Swedish 
<:tiynii8t,  not  to  mention  that  he  seems  to  have  tried  experiments 
similarto  those  which' I  have  made  myself,  and  found  the  result  to 
be  as  I  have  stated  it.  Collection  Acad€mique,  torn.  xi.  p.  6.  et  seq. 
4to.  Paris,  1172. — See  also  the  Probability  of  reaching  the  North 
Pole  discussed. 


-•-^ 


'^- 


#^ 


,# 


SW'" 


-fj-jf  ^^^i^^^^^^^j^^^^P^ 


^H- 


A*#r 


132 


ON  APPROA^      ING 


"January  2d,*  1776.    A  gallon,  Winchester  mea- 
sure, of  sea  water,  which  I  had  fresh  imported  from 
Mr.  Owen  in  Fleet-Street,  was  placed  in  a  shallow 
dish, of  Welsh  ware,  glazed  yellow;  the  depth  of  the 
water  was  three  inches  and  a  half  in  this  shallow 
dish,  which  I  marked  A,  and  placed  on  a  brick  wall 
eight  feet  high  above  the  ground  behind  my  house 
This  wall  on  the  Eastern  side  faces  the  gardens 
belonging  to  five  or  six  houses  in  the  same  street  with 
mine ;  and  on  the  Western  Lide  of  it  is  the  area 
between  my  house  and  the  elaboratory ;  and  West- 
ward of  my  area  is  the  garden  of  Messrs.  Wedgwood 
and  Bentley,    which  I  believe  is  forty  feet  wide, 
bounded  on  the  West  by  high  buildings. 

*^  At  the  same  time  I  placed  another  gallon  of  the 
same  sea  water  in  a  glass  body.  The  column  of 
water  in  this  vessel  was  about  thirteen  inches  high, 
about  six  inches  diameter  at  the  base,  and  about 
three  inches  at  the  mouth  of  the  vessel.  I  placed 
this  body  with  the  sea  water  close  by  the  vessel 
marked  A;  so  that  both  were  equally  distant  from 
the  adjoining  houses;  and  after  marking  the  glass  body 
B,  I  covered,  the  vessels  A  and  B  with  glass  basoiis 
in  such  a  manner,  that  the  air  might  communicate 
with  the  surface  of  the  water,  but  rain  or  snow  might 
be  excluded.  '^f^r  -i^'- 

*'A  Thermometer  was  placed  between  these 
vessels.  .  <  -      •%;    ;;"'^   i^.-'  - 

«  From  the  2d  to  the  7th  of  January,  the  mercury 
in  the  thermometer  stood,  at  various  times,  as  low  as 

*  Mr.  Naime  began  his  experiments  at  the  latter  end  of  this 
Inootb. 


,R;. 


«l 


m 


n 


Mi. 


THE  NORTH  POLE. 


133 


:ir  end  of  this 


31°  of  Fahrenheit;  and  Thames  water,  in  shallow 
wooden  vessels,  placed  on  the  ground,  near  the  wall 
above-mentioned,  was  often  frozen  to  the  thickness 
of  a  crown  piece.  Bat  an  earthen  oil  jar  containing 
twenty  gallons  of  Thames  water,  and  a  like  jar  con- 
taining twenty  gallons  of  distilled  water,  and  each 
covered  with  a  pewter  dish,  preserved  the  water 
contained  in  them  from  freezing  during  this  interval. 

« About  the  7th  of  January,  the  mercury  in  the 
course  of  twenty-four  hours  did  not  rise  above  31**, 
but  sometimes  sunk  to  30°.     Ice  was  formed  in  the 
vessel  marked  A,  but  none  in  the  vessel  marked  B. 
Ice  was  at  the  same  time  formed  in  the  great  jars 
containing  Thames  water  and  distilled  water ;  and  ta 
a  thickness  much  greater  in  the  Thames  water  than 
in  the  water  distilled.    The  ice  obtained  from  the 
vessef  A  was  all  formed  on  the  surface  of  the  water ; 
and  consisted  of  thin  laminae  adhering  to  each  other 
weakly,  and  intercepting  in  their  interstices  a  small 
portion  of  water,   which  was  saline  to  the  taste. 
This  ice,  beaten  gently  with  a  glass  pestle  to  divide 
the  laminae,  then  drained,  and  then  washed  in  dis- 
tilled water,  tasted  like  the  ice  of  fresh  water;  and  ^ 
being  placed  in  a  glass  funnel  before  a  culinary  fire,  ^ 
so  that  the  w'ater  might  drain  oiT  as  soon  as  formed, 
it  dissolved  in  half  an  hour,  and  not  in  less  tidie, 
although  the  thermometer  placed  at  the  same  dis- 
tance close  to  the  funnel  rose  to  a  hundred  and  sixty; 
and  the  side  of  the  funnel  next  to  the  fire  was  hot  to 
the  like  degree,  as  nearly  as  could  be  ascertained  by 
the  touch.    The  water  of  the  ice  thus  melted  was 
fresh  and  palatable,  and  measured  half  a  pint. 


n 


>.\ 


•«i 


^i 


'fK^^i 


«pi»»>ffcj" 


m 


«A 


'.i/ 


^-sH- 


■r~: 


4t* 


134  ^  ON  APPROACHING  «» 

**  From  the  9th  of  January  to  the  11th  inclusive, 
'the  mercury  rose  some  days  to  forty,  and  during 
three  or  four  hours  on  other  days  it  sunk  and  re- 
mained at  thirty,  and  sometimes  for  an  hour  or  less 
it  sunk  to  twenty-nine.  But  it  did  not  remain  at 
thirty  during  any  of  these  days  for  more  than  four  or 
five  hours,  unless  at  the  hours  of  rest,  when  no  ob- 
servation was  made.  During  this  period,  a  thin  coat 
of  ice,  like  the  former,  was  produced  on  the  water 
in  the  shallow  vessel  A ;  but  no  ice  was  formed  in 
the  vessel  B. 

"  January  12,  the  thermometer  pointed  for  several 
hours  between  thirty-one  at  the  highest,  and  twenty- 
nine  at  the  lowest.  A  thick  crust  of  ice,  of  the 
'texture  before  described,  was  formed  in  the  vessel 
A.  This  ice,  broken,  washed,  and  dissolved,  became 
fresh  water,  measuring  a  pint  or  more.  This  quan- 
tity of  ice,  placed  in  a  funnel  before  a  fire,  in  the 
circumstances  eilready  described,  was  not  all  dis- 
solved in  an  hour  and  ten  minutes.  No  ice  was 
formed  in  the  vessel  B.* 

"  January  the  13th  at  night,  and  14th  in  the  morn- 
ing, the  thermometer  sunk  for  some  hours  below 
twenty-seven,  and  did  not  rise  during  sixteen  hours 
above  twenty-eight.  The  water  in  the  vessel  A, 
_  remaining  after  the  foregoing  congelations, '  was 
frozen  to  the  thiclgiess  of  a  quarter  of  an  inch  in 


% 


*  "  The  foregoing  observations  were  committed  to  writing  on 
the  days  when  they  were  respectively -made,  but  the  day  of  the 
mouth  was  not  theu  accurately  noted.  It  may  therefore  be  found 
that  I  have  placed  some  of  the  foregoing  temperatures  a  day  before 
•r  after  that  on  which  they  were  observed." 


Y'"^'- 


THS  NORTH  POLK. 


135 


the  centre,  and  three  quarters  ,of  an  inch  in  the  cir- 
cumference ;  but  no  ice  was  formed  at  any  greater 
depth  in  the  water.  This  ice,  like  the  former,  was 
laminated,  and  when  bruised  and  washed,  it  formed 
frQsh  water  to  the  quantity  of  three  pints. 

<*  On>  the  same  day,  viz.  14th  of  January,  in  the 
morning,  the  thermometer  pointii%  below  twenty- 
seven,  the  Thames  water  in  the  great  jar  was  frozen 
to  the  thickness  of  three  or  four  inches,  if  not  more, 
contiguous  to  the  jar  and  the  surface.  The  distilled 
Thames  water  in  the  other  jar  was  frozen  to  the 
thickness  of  two  inches,  or  thereabouts,  and  con- 
tiguous to  the  jar  and  surface  of  the  water ;  and  the 
sea  water  in  the  glass  body  marked  B  was  for  the 
first  time  frozen.  On  the  surface,  and  in  the  centre 
of  this  surface,  the  ice  was  half  an  inch  thick ;  at  the 
circumference  it  was  an  inch  thick;  and  from  the 
circumference  and  surface  the  ice  formed  contiguous 
to  the  glass,  in  such  a  manner,  that  the  crust  was  an 
inch  thick  near  the  glass  and  surface ;  but  as  it  pro- 
ceeded downwards  towards  the  wider  part  of  the 
glass,  it  tapered  to  an  edge,  terminating  within  an 
inch  of  the  bottom  of  the  vessel.  ^i 

^'  Thds  all  the  ice  was  formed  on  the  surface  and 
contiguous  to  the  glass,  and  was  thickest  where  the 
vessel  was  narrowest ;  that  is  the  quantity  of  ice  was 
inversely  as  the  diameter  of  the  vessel.  This  ice 
resembled  that  obtained  in  the  shallow  vessel  in  its 
laminated  structure  and  sponginess,  and  in  its  enve-. 
loping  a  portion  of  the  salt  water,  with  this  difference 
only,  that  the  laminae  shot  vertically,  and  from  the 
circumference,  inclining  towards  the  centre,  not  di- 


1  ^i 


. 


^ 


136 


■^4  '*'^.■)tj[^^> 


ON  APPROACHING 


IT   \ 


J     :i 


.^.:-      V: 


'^■i  n 


.N^ 


rectly,  but  so  as  to  form  ivith  the  centre  an  angle  of 
about  fifteen  degrees.  This  ice,  bruised  and  washed, 
#  melted  to  a  pint  and  a  half  of  pleasant  fresh  water. 
The  time  and  heat  were  nearly  the  same  as  I  de> 
scribed  above.  , 

**■  Mr.  Barrington,  at  this  and  former  periods  ob- 
served, that  the  Separation  of  the  laminae  of  the  ice 
by  bruising  accelerated  the  effect  produced  by 
washing ;  that  is,  the  extrication  of  the  intercepted 
brine. 

"  January  the  19th  at  night,  the  mercury  in  the 
thermometer  sunk  to  twenty-six.  The  sea  water, 
remaining  after  the  foregoing  congelations  in  the  flat 
dish  marked  A,  was  frozen  so  far,  that  only  a  pint 
remained  fluid  at  the  bottom.  This  ice  was  in  all 
respects  like  the  former  portions.  Bruised,  washed, 
and  pelted,  as  on  former  occasions,  it  gave  a  quart 
of  fresh  water.  At  the  same  time  the  water  in  B  was 
frozen  in  the  manner  before  described,  but  in  a 
larger  quantity,  and  some  laminae  of  ice  shot  close  to 
the  glass  as  far  as  the  bottom  of  the  vessel.  This  ice 
bruised  and  washed  as  formerly,  and  placed  before 
the  fire  in  a  glass  funnel,  melted  in  a  heat  of  a  hun- 
dred and  sixty,  in  an  hour  and  a  half,  to  oile  quart 
of  fresh  water. 

»'  January  the  20th,  the  mercury,  which  stood  at 
twenty-seven  in  the  morning,  and  fell  to  twenty-six 
towards  twelve  o'clock,  fell  in.  a  few  hours  to  twenty- 
four,  and,  before  nine  at  night,  fell  to  twenty-three. 
Only  a  thin  coat  of  ice  was  formed  on  the  water  in 
A,  which  I  did  not  disturb,  expecting  It  to  freeze 
deeper  during  the  night.    The  water  in  the  vessel 


I 


TH 


s> 


THE  NORTH  POLE. 


137 


B  was  frozen  to  some  thickness  at  the  surface,  and 
contiguous  to  the  sides  of  the  glass  body,  but  not  at 
the  bottom.  Expecting  a  stronger  congelation,  I 
suffered  this  also  to  stand  until  the  next  morning,  and 
consequently  could  not  determine  the  quantity  of  ice 
formed  in  it,  otherwise  than  by  feeling  near  the 
surface,  whereby  I  presumed  the  quantity  of  ice  to 

'  be  equal  to  that  last  obtained,  and  formed  in  the 
same  manner.  ,v;jv  >     . 

"  January  the  21st  in  the  morning,  the  thermome- 
ter pointed  to  twenty-eight.  The  thin  crust  of  ice, 
observed  on  the  preceding  night,  did  not  appear  to 
be  increased  or  diminished  in  the  vessel  marked 
A.  The  laminae  of  this  ice  adhered  so  weakly,  that 
the  whole  crust  could  not  be  raised  without  breaking. 
This  ice,  bruised  and  well  washed,  dissolved  to  near 
half  a  pint  of  water,  brackish  to  the  taste.  And  the 
same  day,  in  the  morning,  the  ice  in  B  was  removed, 
bruised,  and  washed  ;  it  melted  to  a  pint  or  more  of 
fresh  water.'* 

..iv"  From  the  21st  to  the  26th  of  January,  the  water 
in  the  vessel  marked  B  was  frozen  twice,  and  the  ice 
formed  each  time  was  bruised  and  washed,  and 
melted  to  fresh  water,  both  portions  measuring  one 
pint  or  more.  "^  • '■' ' ';:f^ 

.•  "  From  the  26th  of  January  at  sun  set,  to  the  27  th 
at  eleven  o'clock  in  the  morning,  the  mercury  in  the 
thermometer  stood,  at  the  usual  hours  of  observation, 
between  twenty  and  eighteen.  The  water  remaining 
after  the  foregoing  congelations  in  B  was  frozen  so 
far,  that  only  half  a  pint  remained  fluid.    Th«  ice, 

18 


t 


.■*s»''  ■' 


1 


^* 


.l^. 


■?' 


%1 


** 


138 


ON  APPROACHING 


bruised,  washedf  and  dissolved,  tasted  a  little  brack- 
ish,  and  measured  one  pint  and  a  half. 

"  On  the  28th  of  January  the  mercury  stood  in  the 
morning  and  until  four  o'clock  in  the  afternoon  be- 
tween twenty-two  and  nineteen,  and  before  eleven 
o'clock  at  night  it  sunk  to  seventeen.  Very  little  ice 
was  formed  in  the  ves>6e\  B ;  and  what  was  formed 
very  easily  crumbled  or  fell  to  small  flakes  in  at- 
tempting to  take  it  out.  I  therefore  suffered  it  to 
remain  in  the  liquor  until  the  morning. 
.  "  On  the  29th  of  January  the  mercury  stood  be- 
tween twenty  and  twenty-two  until  six  o'clock  j  and 
between  twenty  and  nineteen,  from  six  until  twelve 
at  night.  The  quantity  of  ice,  formed  on  the  pre- 
ceding day,  was  not  notably  augmented  or  diminished; 
bruised,  washed,  and  melted,  it  yielded  two  ounces 
of  water,  brackish  to  the  taste,  in  a  greater  degree 
than  any  of  the  foregoing  portions  which  were 
washed. 

"  On  the  30th  of  January,  finding  that  the  tempera- 
ture of  th^  preceding  evening,  of  the  night,  and  of 
this  day,  which  was  between  nineteen  and  twenty- 
one,  had  caused  no  notable  congelation  in  the  small 
quantity  .of  water  remaining  in  B;  finding  also  that 
the  residue  of  the  water  in  A  admitted  of  no  farther 
congelation  worth  notice ;  and  considering  that  the 
slender  laminse  of  ice,  lately  formed  in  these  waters, 
melted  to  salt  water,  and  consequently  that  no  farther 
congelation,  capable  of  separating  the  fresh  water 
from  the  brine,  even  with  the  assistance  of  washing, 
could  take  place ;  I  mixed  the  concentrated  brine  in 
A  with  that  in  6,  and  found  both  scarcely  measured 


4i 


^^ 


<*t 


THE  NORTH   POLE. 


139 


a  wine  pint ;  some  small  crystals  were  found  in  the 
bottom  of  both  vessels,  which  sunk  in  the  brkie,  and 
were  to  the  taste  sea  salt.  It  is  hence  evident  that 
some  sea  salt  is  formed  in  crystals  by  the  concentra* 
tion  produced  by  cold  acting  gradually,  and  causing 
congelation  only  on  the  surface  of  the  water,  or  not 
affecting  that  part  of  it  which  is  contiguous  to  the 
bottom  of  the  vessel. 

*^  The  quantity  of  these  crystals  of  sea  salt  was 
about  two  grains.  I  poured  them  together  with  the 
water  into  a  china  plate,  set  in  a  sand  heat,  and,  by 
crystallization,  obtained  sea  salt  and  the  other  saline 
contents  of  sea  water,  in  a  dry  form,  near  two  ounces, 
avoirdupois. 

"  Now,  as  this  quantity  of  sea  water  (that  is,  two 
gallons)  taken  on  our  coast,  generally  yields  about 
seven  ounces  of  saline  matters,  it  appears,  that  two- 
thirds  or  more  of  the  sea  salt,  and  bitter  salts  of  sea 
water,  are  intercepted  in  the  ice  of  the  successive 
congelations,  and  are  washed  away  by  fresh  water, 
applied  as  above-mentioned.  Hence  we  learn  that 
sea  water  may  be  freshened  by  freezing,  provided 
the  brine  enveloped  between  the  laminae  of  its  ice  be 
washed  away.  And  in  cold  countries  salt  might  be 
prepared  from  sea  water  at  a  very  moderate  expense ; 
for  by  freezing  shallow  ponds  of  this  water,  by  turn- 
ing the  ice  to  drain  off  the  brine,  and  when  the  brine 
is  reduced  to  a  twentieth  part  or  less  by  evaporation, 
very  little  evaporation  and  fuel  will  be  necessary 
towards  the  formation  of  the  salt*    But  all  the  salt 


-5*: 


k 
•^ 


f 


** 

,* 


#• 


*  "  Wallerius  says,  this  art  is  practised  in  the  Northern  coun* 

tries." 


P 


l* 

i'-^ 


r  -» 

\  , 


.'Si«t 


^ 


•\ 


.;» 


lif 


140 


ON  APPROACHING 


# 


i^'t  'W 


of  the  sea  water  employed  will  not  be  obtained, 
because  the  greater  part  of  it  will  be  retained  be- 
tween the  laminae  of  the  ice,  which  must  be  re- 
jected; and  the  concentration  by  freezing  cannot 
be  advantageously  carried  farther  than  is  above 
expressed,  because  at  that  degree  of  concentration 
the  cold,  and  the  time  necessary  to  cause  farther 
congelations,  must  be  very  considerable,  as  will  the 
waste  of  salt  likewise,  since  the  ice  is  then  strongly 
saline. 

"  A  small  portion  of  the  ice,  taken  at  various  times 
from  B  since  the  26th  of  January,  was  not  washed, 
but  only  left  to  drain  in  a  funnel ;  and  each  portion 
thus  drained  during  five  or  six  days,  being  Separately 
dissolved,  tasted  strongly  of  salt,  although  the  like 
ice,  which  was  bruised  and  washed,  yielded  fresh 
water.  This  proves  that  washing  removes  the  inter- 
cepted brine ;  and  that  this  brine  does  not  separate 
by  draining.  ^.' 

«  January  the  20th,  at  eight  o'clock  in  the  evening, 
the  thermometer  pointing  at  twenty-three,  in  the  open 
air  where  the  thermometer  stood,  I  mixed  snow  with 
smoking  spirit  of  nitre,  and  placed  in  the  mixture  a 
glass  half  pint  tumbler  full  of  sea  water ;  and  at  the 
same  time  placed  the  thermometer  in  the  mixture. 
In  two  minutes  the  mercury  sunk  out  of  the  tube 
quite  into  the  globe.  The  scale  extends  only  twenty- 
five  degrees  below  0  of  Fahrenheit;  wherefore  I 
could  not  determine  how  many  degrees  lower  it 
would  have  sunk  on  a  more  extended  scale.  In  five 
minutes  some  slender  laminae  of  ice  began  to  shoot 
from  the  circumference  of  the  water,  and  adhered  to 


?»•/■• 


I 


tit-i   :rWc>:, 


-e-V 


.^' 


THE  NORTH  POLE. 


141 


the  glass.  The  whole  water  was  not  frozen  in  less 
than  an  houTy  at  which  time  the  mercury  in  the  ther- 
mometer rose  to  twenty  degrees  below  0.  Having 
another  mixture  of  the  same  kind  ready  made,  I 
briskly  removed  the  tumbler  with  the  ice  it  contained 
into  the  fresh  mixture,  which,  like  the  former,  sunk 
the  mercury  into  the  globe. 

"  The  ice  of  sea  water  is  more  opaque  than  that  of 
fresh  water,  when  both  are  naturally  congealed. 
For  the  elastic  fluid  in  common  water  forms  bubbles 
only  in  the  central  parts  of  the  water  last  frozen ; 
but  the  ice  of  sea  water  consists  of  alternate  parts  of 
ice  and  brine;  the  density  of  which  being  unequal, 
and  the  matter  of  them  being  also  dissimilar,  light 
cannot  be  freely  transmitted,  but  ^s  partly  reflected 
and  refracted,  according  to  Sir  Isaac  Newton's  ideas 
of  light. 

"  In  the  experiment  last  mentioned,  the  ice  was 
commonly  opaque ;  and  when  it  was  exposed  to  the 
fresh  frigorific  mixture,  it  became  like  a  mass  of  snow 
compressed,  having  a  snowy  whiteness  and  opacity, 
perfect  near  the  surface,  but  not  perfect  toward  the 
bottom. 

"  The  tumbler,  with  the  ice  it  contained,  was  kept 
in  this  last  mentioned  mixture  an  hour,  when  the 
mercury  denoted  that  no  farther  degree  of  cold  could 
be  given  by  this  mixture.  The  tumbler  was  then 
placed  in  snow  until  the  next  day,  to  preserve  the 
ice  for  farther  observation.  Nothwithstanding  the 
extreme  cold  to  which  it  had  been  so  long  exposed, 
and  the  cold  medium  in  which  it  was  placed,  the  ice 
was  not  solid  hke  that  of  fresh  water,  but,  on  the 


H2 


WN  APPROACIIIKO 


..*,  *     '. 


|«i-': 


contrary,  could  easily  be  cut  through  the  centre  of 
the  mass  with  a  knife.  The  ice  tasted  equally  of  salt 
through  the  whole  masSf  in  the  same  manner  as  a 
like  quantity  of  sea  water.  Bruised  briskly,  washed 
as  already  described,  and  melted,  it  yielded  fresh 
water  to  the  quantity  of  four-fiilhs  of  the  water  frozen; 
wherefore  in  washing  very  little  ice  was  dissolved 
whilst  the  salt  water  intercepted  in  the  ice  was 
removed. 

»'  Mr.  Barrington  having  observed  that  an  artificial 
freezing  commences  from  the  bottom  and  sides  of  the 
mass  of  water  placed  as  usual  in  the  frigorific  mix- 
ture, but  that  natural  freezing  commences  on  the 
surface  and  proceeds  downward ;  and  it  occurring  to 
me  that  the  specific  gravity  of  incongelablc  brine  is 
greater  than  that  of  the  congelable  water;  and,  con- 
sequently, that  this  greater  specific  gravity  favours 
the  separation  of  brine  from  the  ice  of  sea  water, 
when  the  freezing  commences  on  the  surface  of  sea 
water,  and  may  be  an  impediment  to  the  separation 
of  the  incongelablc  brine  from  the  ice  artificially 
formed  in  the  sea  water,  when  the  congelation  pro- 
ceeds from  the  bottom  upwards :  on  these  considera- 
tions it  seemed  that  the  foregoing  experiments  indi- 
cate, that  ice  formed  in  sea  water  cannot,  when 
melted,  become  fresh  water,  unless  it  be  washed  in 
fresh  water ;  but  do  not  fully  prove,  that  ice  formed 
on  the  surface  only,  and  proceeding  slowly  down- 
wards, in  sea  water,  may  not  consist  of  fresh  water, 
and  be  freed  from  brine,  by  reason  of  the  specific 
gravity  of  brine  and  other  unnoticed  circumstances. 
Therefore,  on  the  21  st  of  January,  at  two  o'clock. 


.-;3^  ^  "!|t-r^'*..^-i'i 


■■-:ill<K^.'^9*^..f^ 


''^•7'^ZS^^ 


^ 


THE  NORTH  POLR. 


143 


when  the  mercury  stood  in  the  open  ftir  at  twenty- 
nine,  I  made  the  following  experiment,  with  a  view- 
to  determine  whether  sea  water,  frozen  artificially 
from  the  surface  downwards  in  the  manner  performed 
by  nature,  would  not  yield  ice  of  a  solid  texture 
capable  of  melting  to  fresh  water  without  washing, 
merely  by  draining ;  which  must  take  place  in  moun- 
tains of  ice,  if  any  are  formed  in  the  Northern  Sea; 
because,  ice  being  specifically  lighter  than  water, 
and  the  access  of  congealed  water  being  at  the  base, 
the  portions  first  frozen  will  be  raised  above  the  water 
by  succeeding  portions  frozen,  and  thus  a  mountain 
of  ice  may  be  raised,  whose  mass  and  height  above 
water  will  be  to  the  massive  base  immersed  in  water, 
inversely  as  the  specific  gravity  of  ice  is  to  that  of 
water. 

**1  placed  therefore  a  gallon  of  sea  water  in  a 
glazed  earthen  vessel,  whose  diameter  was  one  third 
greater  than  the  depth  of  the  water.  In  this  water  I 
slung  a  thin  glass  bason,  cut  from  a  bolt  head,  capa- 
ble of  containfng  near  two  quarts  of  water,  in  such 
i%inner  that  it  might  be  immersed  two  inches  deep 
in  the  sea  water.  The  vessel  containing  the  sea 
water  was  surrounded  with  snow.  I  then  filled  the 
bason,  which  was  suspended  in  the  sea  water,  with 
snow  pressed  down  with  a  glass  pestle,  and  poured 
into  the  snow  the  usual  quantity  of  strong  nitrous 
acid.  ^,    ^    _^^   ,  ,^^ 

"In  fifteen  minutes  some  crystals  of  ice  were  formed 
on  the  interior  glass  bason,  in  the  part  where  it  was 
contiguous  to  the  surface  of  the  sea  water.  In  three 
hours  the  whole  bottom  of  the  bason,  containing  the 


.  d 


,n 


I 


.f^'.i 


J' 


I. 


4^ 


144 


trtiiUf'^, 


ON  APPROACHING 


t 


U      i      . 


frigorific  mixture,  was  coated  with  ice,  thg  thickness 
of  which  was  half  an  inch  or  less  at  the  bottom  of 
the  bason,  increasing  to  three-fourths  of  an  inch  at 
the  part  which  corresponded  with  the  surface  of  the 
water. 

"I  easily  "separated  it  entire  from  the  bason, 
found  it  somewhat  firmer  in  its  aggregation  than  the> 
ice  slowly  formed  by  natural  freezing,  and  not  com- 
posed of  laminae  like  this  latter,  but  similar  in  tex- 
ture to  the  salt  water  frozen  by  artificial  cold  applied 
in  the  usual  manner.  I  placed  it  on  a  heap  of  snow, 
where  it  remained  to  drain  upwards  of  six  hours,  but 
still  was  wet  to  the  touch  on  the  surface,  and  in  the 
fi'esh  surfaces  of  the  fractured  parts.  I  then  placed  a 
part  of  it  in  a  glass  funnel  before  the  fire,  to  melt, 
and  found  the  water  strongly  saline  to  the  taste,  but 
not  near  so  saline  as  equal  parts  of  sea  and  river 
water  mixed. 

«  Another  portion  of  this  ice,  which  was  wrapped/ 
up  in  filtering  paper,  and  left  to  drain  on  a  heap  of 
dry  snow  during  four  days,  when  melted,  was  saline 
to  the  taste,  and  not  sensibly  difierent  from  that 
w:hich  had  drained  only  six  or  seven  hours.  Whence 
it  appeared,  that  ice  formed  in  the  sea  water,  in  cir- 
cumstances similar  to  thpse  which  attend  natural 
congelation,  is,  nevertheless,  saline  to  the  taste.  •  ■ 
•  **  The  several  portions  of  water  obtained  in  the 
foregoing  experiments,  from  the  washed  ice  of  the 
sea  water  in  A  and  B,  being  preserved  in  glass  stop- 
per bottles,  were  not  examined.  Although  they 
were  fresh  to  the  taste,  it  appeared  by  the  quantity 
of  lima  eor:M^  which  they  all  formed  with  saturated 


^^. 


i  mi    iiwi     w 


MHlbW»SeM>-'.' 


* 


« 


THE  NORTH  POLE. 


145 


nitrous  solution  of  silver,  that  they  were  strongly 
impregnated  with  marine  salt,  comparatively  with 
Thames  and  New  River  water,  examined  in  the  like 
manner. 

*'  Mr.  Barrington  observing,  that  salt  in  water  is  an 
impediment  to  the  congelation  of  that  water,  pre- 
sumed, that  salt  in  water  would  accelerate  the  thaw- 
ing of  ice  immersed  in  it;  and  that  in  equal  tempe- 
ratures ice  would  be  thawed  in  sea  water  sooner 
than  in  fresh  water.  I  theiefore  made  the  following 
experiment. 

*^  January  the  20th,  when  the  thermometer  pointed 
to  twenty-three,  about  nine  o'clock  at  night,  I  placed 
five  ounces  and  half  a  drachm,  avoirdupois,  of 
Thames  water  in  a  half  pint  glass  tumbler ;  and  the 
like  quantity  of  the  same  water  distilled  in  another 
half  pint  glass  tumbler  of  equal  figure  and  capacity 
with  the  foregoing.  The  tumblers  were  placed  on 
the  wall  formerly  described,  and  left  there  covered 
with  glass  until  eleven  o'clock  next  morning. 

« In  the  morning,  at  eleven  o'clock,  the  thermome- 
ter pointed  to  twenty-eight.  The  water  in  both  tum- 
blers was  frozen  quite  through,  and  formed  masses  of 
ice,  transparent  as  crystal  in  every  part,  except  the 
centre,  and  near  the  bottom,  which  parts  were  ren- 
dered opaque  to  the  thickness  of  half  an  inch,  by  a 
number  of  air  bubbles  locked  up  in  the  ice.  The 
distilled  water  had  been  kept  several  days  in  the  jar 
above  described,  whose  mouth  was  only  covered 
with  an  inverted  pewter  dish.         •   *     .   ;  ,.; 

"  Into  a  glass  tumbler,  capable  of  holding  a  Win- 
chester pint  or  more  1  put  a  wine  pint  of  Thames 

19 


^ 


'■-i 


I 


M 


146 


t'^  ON  APFROACHING 


Si     • 

-J. 


i'r:.T 


♦i^:- 


water;  and  into  another  tumbler  of  the  same  figure  and 
capacity,  I  poured  a  pint  of  sea  water  concentrL:ed, 
by  freezing  one  fourth  of  it,  the  better  to  represent 
sea  water  of  the  great  oceans,  which  are  not  aiTected 
by  rivers  so  much  as  the  sea  water  used  in  these 
experiments  must  be,  as  it  was  taken  up  near  the 
North  Foreland.    The  sea  water  was  thus  concen- 
trated for  these  farther  reasons :  first,  that  the  effect 
of  salt  in  the  water  might  be  more  conspicuous  dur- 
ing the  thawing  of  the  ice ;  and  secondly,  to  prevent 
the  first  portions  of  ice  thawed  from  diluting  the  salt 
water  to  a  degree  which  never  is  found  in  the  ocean. 
I  reduced  the  sea  and  the  Thames  water,  contained 
in  these  tumblers,  to  the  same  temperature  exactly, 
in  the  open  air ;  then  taking  hold  of  each  by  the  sum- 
mit of  the  glass  above  the  water,  I  carried  them  into 
my  study,  and  placed  them  on  a  carpet  fifteen  feet 
equally  distant  from  the  fire,  and  three  inches  from 
the  wainscot  of  the  wall  opposite  the  fire,  and  equally 
distant  from  a  door .  on  one  side,   and  a  window, 
which  extends  within  fourteen  inches  of  the  floor,  on 
the  other.    The  tumblers  containing  the  frozen  water, 
were  immersed  in  a  large  pan  of  hot  water,  close 
to  each   other,   and  near  the  centre  of  the  pan, 
the  water  rising  to  the  height  of  the  ice  in  the 
tumblers ;  after  a  few  minutes  the  ice  was  thrown 
out,  by  inverting  the  glasses  on  clean  paper.    The 
two  pieces  of  ice  were  equal  in  size,  figure,  and 
weight;     the    weight   of  each   being  five    ounces 
avoirdupois. 

«  The  moment  before  the  ice  was  taken  out  of  the 
tumblers,  I  found  the  temperature  of  the  sea  and 


■'■^^ 


* 


m. 


^ 


.* 


-ss 


e  figure  and 
ncentrcied, 
o  represent 
not  affected 
id  in  these 
ip  near  the 
1U8  concen- 
at  the  effect 
)icuous  dur- 

to  prevent 
ing  the  salt 
m  the  ocean. 
*,  contained 
ure  exactly, 
by  the  sum- 
id  them  into 
it  fifteen  feet 
inches  fi*om 
,  and  equally 
I  a  window, 
the  floor,  on 
frozen  water, 
water,  close 
of  the  pan, 
;  ice  in  the 

was  thrown 

paper.    The 

,  figure,  and 

five    ouncei 

en  out  of  the 
the  sea  and 


i^ 


:  1 


THE  NORTH  POLE. 


147 


fresh  water,  placed  as  above-mentioned, 'to  be  equal,  / 
and  exactly  thirty-four;  the  temperature  of  the  air  in '^ 
that  part  of  the  room  being  forty-six.    I  plunged  the 
pieces  of  ice  immediately,  one  in  the  sea  water,  the 
other  in  the  fresh  water.    It  was  at  this  instant  two  , 
o'clock  in  the  afternoon.    In  ten  minutee  the  tempe- 
rature of  the  sea  water  was  thirty-two,  that  of  the 
fresh  water  was  thirty-three  and  a  half.    In  half  an 
hour  the  sea  water  raised  the  mercury  to  thirty-three  : 
the  fresh  water  raised  it  to  thirty-four  and  a  half. 

«  At  this  instant,  viz.  half  an  hour  past  two  o'clock,  ' 
I  took  both  the  pieces  of  ice  at  the  same  time^ ' 
weighed  them  briskly,  and  replaced  them  in  their 
respective  vessels  at  the  same  instant.    Of  the  ice 
placed  in  the  sea  water,  half  an  ounce  was  dissolved; . 
of  the  ice  placed  in  the  fresh  water,  only  four 
drachms  and  a  half  were  dissolved.  -  • 

"  From  half  an  hour  past  two  o'clock  until  six  I 
fi'equently  changed  the  position  of  the  tumblers, 
making  one  take  the  place  of  the  other.  At  six,  the 
temperature  of  the  sea  water  was  thirty-six,  that  of 
the  fresh  water  was  thirty-seven  and  a  half.  In  the 
manner  already  mentioned,  the  ice  was  at  this  time 
weighed  and  replaced.  Of  the  ice  in  sea  water 
three  ounces  and  four  drachms  were  dissolved ;  of 
that  in  fresh  water,  only  two  ounces  and  eight 
drachms. 

"  It  is  observable,  that  the  sea  water  was  a  degree 
and  a  half  colder,  ever  since  the  immersion  of  the 
ice,  than  the  fresh  water,  acted  on  by  the  like  mass 
of  ice,  and  placed  in  the  like  circumstances ;  and 
nevertheless  the  ice  was  dissolved  much  quicker  in 


i^'is 


t 


t 


I--* 


t 


.*^ 


■ijf? 


148 


ON  APPR0(ACHmO 


\ 


the  colder  sea  water.  The  quicker  solution  of  the 
ice  in  sea  water  was  evidently  the  cause  of  the 
greater  degree  of  cold  preserved  in  it  during  four 

M  hours ;  and  it  already  appeared,  that  salt  water  is  a 
more  powerful  solvent  of  ice  than  fresh  water  in  the 
like  temperature.  And,  agreeable  to  Mr.  Barring- 
ton^s  suggestion,  the  matter  which  impedes  the  con- 
gelation of  water  must  of  course  facilitate  the  thaw- 
ing of  ice.  The  nitrous  acid  furnishes  us  with 
another  strijcing  instance  to  this  efiect ;  for  no  cold 
can  be  produced  to  freeze  the  water  in  it ;  and  a  red 
hot  ladle  cannot  thaw  ice  placed  in  it,  so  quickly  as 
ice  is  thawed  by  nitrous  acid. 

"  At  ten  o'clock,  or  in  eight  hours  after  the  pieces 
of  ice  were  first  placed  in  the  sea  and  Thames  water, 
the  temperature  of  the  sea  water  was  thirty-nine, 
that  of  the  Thames  water  only  thirty-eight.  At  this 
time,  of  the  ice  in  sea  water  four  ounces  eight 
drachms  were  dissolved ;  of  the  ice  in  Thames  water, 
four  ounces  only  were  dissolved.  The  sea  water 
being  at  this  period  warmer  than  the  Thames  water, 
*'  corresponds  with  the  small  portion  of  ice  remaining 
in  it,  compared  with  that  remaining  in  the  fresh 
water.  The  temperature  of  the  room  in  the  place 
where  the  tumblers  stood,  being,  by  reason  of  the 
fire  kept  constantly  in  it,  forty-four  or  forty-five,  for 
the  last  six  hours. 

"  In  twelve  hours,  or  at  two  o'clock  in  the  morn- 
ing, the  temperature  of  the  room  near  the  vessels  of 
water  being  nearly  the  same  as  formerly  described, 
the  temperature  of  the  sea  water  was  forty,  the  tem- 

i  perature  of  the  fresh  water  was  thirty-nine.    Four 


1 


■^- 


.,M. 


J-  >. 


•  * 


THE  NORTH  POLE. 


149 


ition  of  the 

luse  of  the 

during  four 

t  water  is  a 

vater  in  the 

Ir.  Barring- 

les  the  con- 

e  the  thaw- 

es   us  with 

for  no  cold 

;  and  a  red 

0  quickly  as 

r  the  pieces 
tames  water, 
thirty-nine, 
;ht.  At  this 
•unces  eight 
lames  water, 
3  sea  water 
lames  water, 
:e  remaining 
n  the  fresh 
n  the  place 
tason  of  the 
)rty-five,  for 

in  the  morn- 
le  vessels  of 
[T  described, 
ty,  the  tem- 
aine.    Four 


>*4       A 


ounces  fifteen  drachms  '^  the  ice  in  salt  water  were 
dissolved,  only  one  drachm  remaining;  four  ounces 
ten  drachms  of  the  ice  in  fresh  water  were  dissolved, 
only  six  drachms  remaining. 

<•''  At  the  end  of  the  thirteenth  hour,  after  the  im- 
mersion of  the  masses  of  ice  in  the  fresh  and  in  the  salt 
water,  that  is,  at  three  in  the  morning,  the  tempera- 
ture of  the  room  was  forty-five  near  the  place  where 
the  tumblers  stood.  The  temperature  of  the  open  air 
was  thirty-one.  The  ice  in  the  sea  water  was  melted. 
The  quantity  of  ice  remaining  in  the  fresh  water  was 
one  drachm,  which,  in  fifteen  minutes  more,  was 
entirely  melted.  •t"^:-'  ■■ 

,, "  At  this  period,  when  the  ice  in  the  fi^sh  water 
was  melted,  that  is,  a  quarter  of  an  hour  past  three, 
the  mercury  stood  at  forty  in  the  fresh  water,  in  the 
salt  water  it  stood  at  forty-one.  In  a  quarter  of  an 
hour  after  this,  the  mercury  stood  at  forty-two  in  the 
salt  water,  and  at  forty-one  in  the  fresh  water.  In  a 
quarter  of  an  hour  more,  the  temperature  remained 
unalterable  in  the  salt  and  fresh  water,  although  the 
temperature  of  the  air  between  and  near  the  vessels 
was  forty-five,  and  the  vessel  on  the  right  was  placed 
on  the  left.,  and  replaced  several  times.  And  both 
vessels  were  at  all  times  equidistant  from  the  wain- 
scot, which  was  perfectly  close,  as  were  the  boards 
of  the  floor  also.  s  -  ..         .^  ', 

**  In  a  quarter  of  an  hour  more,  the  temperature  of 
the  air  near  and  between  the  tumblers  remained 
forty-five;  the  temperature  of  the  fresh  water  was 
scarcely  forty-two;  the  temperature  of  the  salt  water 
was  forty-two  and  a  half,      v*  i    v.  ^.  ;4f>$;'V 


"61= 


■f     I 


» 


%Vf 


■r,  * 


^^*. 


'*       f      M  — 


m 


m* 


150 


ON  APPR0ACHIK6 


^?4: 


%*" 


i' 


■  .»f  ■: 


hi 


i*   . 


"  In  a  quarter  of  an  hour  nibre,  the  temperature  of 
the  air  between  the  tumblers  being  forty-four  and  a 
half,  the  temperature  of  the  salt  water  was  forty- 
three  ;  the  temperature  of  the  fresh  water  was  some- 
what more  than  forty-two.  It  was  now  past  four 
o^clock  in  the  morning,  on  Monday  the  22d  of 
January.  I  went  to  bed,  leaving  the  tumblers  in  the 
position  described,  ^-j  r,^.    ..>~.     .  , ..,  ^^^  :Aiy  .-.  . 

"  It  was  observed,  during  the  foregoing  and  other 
experiments,  and  it  is  visible,  from  the  experiments 
related,  that  fire,  in  diffusing  itself  from  warm  bodies 
to  contiguous  cold  bodies,  proceeds  slowly ;  that  cold 
bodies  do  not  acquire  the  temperature  of  the  warmer 
medium  in  which  they  are  immersed  so  soon  as  is 
commonly  imagined,  but,  on  the  contrary,  require  a 
considerable  time  for  that  purpose ;  and  this  time  is 
directly  as  the  diameter  of  the  cold  body. 

"  It  was  inferred  from  these  experiments,  that  a 
temperate  body,  like  water,  placed  in  a  cold  medium, 
as  in  air,  cooled  to  thirty  or  thirty-one  of  Fahrenheit, 
requires  many  hours  before  it  acquires  the  tempera- 
ture of  the  surrounding  medium,  and  before  a  conge- 
lation commences ;  and  that  the  time  necessary  for 
tlie  commencement  of  the  congelation  is  directly  as 
the  mass  and  shortest  diameter  of  the  water,  and  the 
progress  of  the  congelation  is  inversely  as  the  depth 
©f  the  water.  ^ 

"It  was  also  observed,  that  as  much  of  let  given 
mass  of  water  was  frozen  in  five  hours  in  a  tempera- 
ture of  twelve  degrees  below  the  freezing  point,  as 
was  frozen  in  one  hour  in  a  temperature  fifty  d^reeS 


'V 


m 


,f 


I 


i» 


,j|. 


^^' 


TItE  NORTH  POLE. 


131 


below  the  freezing  point ;  and  that  long  duration  of 
the  temperature  between  twenty  and  thirty-two  is, 
towards  the  congelation  of  water,  equivalent  to  inten- 
sity of  cold,  such  as  is  marked  0,  and  below  0,  in 
Fahrenheit,  but  of  short  duration.  ^ 

« It  was  moreover  observed,  that  water  in  thick 
jars  covered  was  not  frozen,  when  water  in  open 
vessels  was  frozen ;  that  water  included  in  massive 
vessels  of  wood,  or  surrounded  by  any  matter  except 
water,  to  some  thickness,  preserved  its  temperature, 
and  resisted  congelation,  longer  than  the  like  quan- 
tity of  water  exposed  to  the  cold  air ;  and  that  water 
in  thick  vessels  was  not  frozen  so  soon  as  a  like 
quantity  of  water  in  thin  vessels  of  like  matter,  figure, 
and  capacity.  It  was  thence  inferred,  that  fire  does 
not  so  quickly  pervade  thick  bodies  as  it  does  thin 
bodies;  and  that  fire  pervades  water  more  freely 
than  it  does  solid  bodies,  and  sooner  diffuses  itself 
from  water  to  air,  than  from  any  other  body  contain- 
ing water  to  air.  ^'.V'-..    ^^#'^'   l'V>.'''^**^'^:<!'>'    'TJ*     . 

"  Thence  it  followed,  that  in  reasoning  on  the  phe^ 
Bomena  of  congelation,  the  masses  of  water,  the 
duration  of  cold  temperature  in  the  atmosphere,  and 
the  masses  of  other  matter  surrounding  water,  are  to 
be  considered.  Deep  rivers  and  lakes  do  not  fi-eeze 
so  soon  as  shallow  rivers  and  lakes.  Large  bodies 
of  water  are  never  frozen  in  any  temperature  of 
short  duration ;  but  shallow  waters  are  often  frozen 
in  the  summer.  >i  »v  • 

"It  need  not  be  presumed,  that  certain  lakes 
which  are  never  frozen,  communicate  with  subterra- 
neous fires,  or  hot  mineral  streams ;  or  that  they  ar« 


«»■ 


*  X' 


f  f 


m. 


*/ 


f 


f^  *  i* 


'•*' 


^A 


i 


'. 


N 


1" 


V  ,/ 


■1 


>        » 


152 


ON  APPR0ACHIK6 


'!! 


impregnated  with  matter  which  impedes  congelation: 
but  it  is  rather  to  be  presumed,  that  as  fire  slowlj 
pervades,  enters,  or  quits  bodies,  the  time  necessary 
for  its  diffusing  itself  from  deep  lakes  to  the  cold 
atmosphere  is  greater  than  ever  such  temperature  of 
the  atmosphere  continues  without  intermission  below 
the  freezing  point.  .*"  v   ^     ■ 

«  By  the  like  reasoning  applied  to  masses  of  earth 
and  other  matter,  which  are  not  so  quickly  pervaded 
by  fire  as  water  is,  we  can  conceive  why  deep  wells 
and  springs  at  or  near  their  issuing  from  the  earth 
are  not  frozen  in  this  climate,  even  when  navigable 
rivers  are  ice-bound.  We  also  understand  why  the 
main  pipes,  buried  in  our  streets,  retain  the  water 
fluid,  when  the  pipes  leading  from  these  to  the 
houses,  and  crossing  the  area  of  each  house,  arc 
choked  with  ice ;  and  why  hay  bands  twisted  round 
these  small  pipes  prevent  the  freezing,  &c. 

"  On  these  grounds  it  is  presumed,  that  no  consider- 
able congelation  ever  takes  place  in  the  sea,  because 
this  is  the  greatest  and  deepest  mass  of  water  we 
know  of;  because  it  is  always  in  motion,  and  commu- 
nicates with  the  water  of  temperate  climates ;  because 
sea  water  is  not  so  easily  frozen  as  fresh  water; 
because  the  ice  found  in  the  sea  is  solid,  and  in 
transparency  not  different  from  the  ice  of  fresh  water; 
and,  lastly,  because  this  floating  ice,  which  is  met 
with  by  navigators,  both  in  high  Northern  and  South- 
ern latitudes,  when  melted,  is  palatable  to  the  taste ; 
whereas  the  ice  formed  from  sea  water  is  very  saline, 
if  it  be  thawed  without  having  been  washed  in  fresh 
M'ater.  .    .  ,  _ 


•^. 


#' 


S-' 


THE  NORTH  POLE. 


153 


«*  It  is  also  presumed,  that  in  the  deep  Northem 
seas  the  water  near  the  surface  will  be  found  warmer 
than  that  near  the  bottom  at  the  approach  of  sum- 
mer ;  and  will  be  found  colder  near  the  surface  than 
at  the  bottom  in  the  first  month  of  the  cold  season, 
for  the  reasons  already  expressed :  and  in  like  man- 
ner, that,  during  the  first  six  or  eight  hours  of  a  frost 
in  England,  the  water  in  any  deep  lake  will  be  found 
eolder  near  the  surface  than  at  the  bottom,  but  that 
the  water  at  the  bottom  will  be  found  colder  than 
that  near  the  surface  in  twenty-four  hours  afler  a 
thaw,  provided  the  air  be  temperate,  or  nearly  so." 

It  having  been  proved,  from  what  hath  been  already 
urged,  as  well  as  b"  the  preceding  experiments  of 
Dr.  Higgins,  that  the  floating  ice,  which  is  observed 
both  in  high  Southern  and  Northern  latitudes,  qannot 
be  probably  formed  from  sea  water,  it  may  be  thought 
incumbent  upon  me  to  show  how  such  quantities  can 
be  supplied  from  springs,  rain,  or  frozen  snow. 

The  rivers,  which  are  always  found  at  certain 
intervals  in  any  large  tract  of  land,  undoubtedly  sup- 
ply considerable  part  of  such  ice ;  but  there  are  not 
wanting  other  sources  from  which  these  floating 
masses  may  be  produced.     "     - 

The  larger  and  higher  ice  islands*  I  conceiv  to 
be  chiefly  formed  on  shore,  after  which  they  are 

*  Mr.  Wales  observes,  that  in  the  islands  of  ice,  near  Georgia 
Australia  and  Sandwich  Land,  there  are  strata  of  dirty  ice,  wbicb 
irrefragably  proves  their  having  been  formed  on  the  land. — Remarlcs 
on  Dr.  Forster's  Account,  &c.  8vo.  London,  1778,  p.  106. 

With  regard  to  the  formation  of  ice  islands,  see  likewise  Capteini 
Cook's  Voyage,  vol.  ii.  p.  213  4ld  240;  vlho  conceiv6»  tiiem  t« 

•     20 


^-s 


i 


J    i 


ii 


^ 


1     i3 
■  /? - 


,.  ,*. 


154 


ON  APPROACHING 


•* 


Jf^, 


'  "    ^ 


r 


^  \ 


1*     >,• 


undermined  by  the  rills  and  melted  gnow,  during  the 
summer,  of  which  we  have  an  accurate  account 
in  the  late  voyage  towards  the  North  Pole.* 

arise  from  congealed  snow  and  sleet  in  the  valleys.  Captain  Cook 
also  supposes,  that  the  ice  cliffs,  at  the  end  of  these  valleys,  often 
project  a  great  way  into  the  sea,  when  they  are  sheltered  from  the 
violence  of  the  wind,  p.  242. 

*  "  Large  pieces  frequently  break  off  from  the  ice^bergs,  and 
fall  with  great  noise  into  the  water :  we  observed  one  piece  which 
had  floated  out  into  the  bay,  and  grounded  in  twenty-four  fathoms ;  it 
was  fifty  feet  high  above  the  surface  of  the  water,  and  of  the  same 
beautiful  colour  as  the  ice-berg."  p.  70. 

I  have  likewise  been  favoured  with  the  following  account  of  ice- 
islands  on  the  coast  of  Labrador,  from  Lieutenant  John  Cartwright, 
of  the  Royal  Navy,  to  whom  I  have  not  only  this  obligation. — See 
the  Probability  of  reaching  the  North  Pole,  p.  8. 

"  Dear  Sir,  "  Thursday,  Feb.  28,  1776. 

"  In  conformity  with  my  promise  of  yesterday,  I  now  send  you, 
88  nearly  as  I  can  recollect,  my  brother's  account  (who  hath  resided 
four  years  on  the  Labrador  coast)  of  the  formation  of  those  great 
massesof  frozen  snow,  seen  annually  in  very  great  numbers  on  the 
Northern  coast  of  America,  and  by  mariners  usually  culled  hlands 
of  ice. 

"  Along  the  coast  of  Labrador,  the  sea,  in  winter,  is  frozen  to  a 
great  distance  from  the  land.  The  Northwest  is  the  prevailing  and 
coldest  wind.  The  snow,  carried  by  this  or  any  other  Westerly 
winds  over  the  cliffs  of  the  coast,  falls  becalmed  upon  the  ice  at  the 
foot  of  the  said  cliffs,  drifting  up  to  the  very  tops  of  them,  although 
many  of  them  are  not  inferior  to  that  of  Dover,  or  those  about  Lul- 
worth.  The  current  of  the  strong  Western  winds  having  passed 
these  precipices,  takes  its  course  downwards  into  the  undisturbed 
air  below ;  but  it  is  not  until  it  arrives  at  some  distance  from  the  land, 
that  it  can  be  felt  on  th<  jrface  of  the  sea.  Having  the  frozen  sur- 
face of  the  sea  for  a  base,  and  the  precipice  for  a  perpendicular,  an 
bypothenuse  is  made  by  the  descending  direction  of  the  wind.  The 
inclosed  triangle,  be  the  clifis  ever  so  high,  will  be  filled  with  snow ; 
because  the  tops  of  the  adjoining  hills  being  quite  naked,  are 


t 


i-.a*"*©* 


'tmiuM^ 


THE  NORTH  POLE. 


% 


155 


during  the 

te  account 

« 

Captain  Cook 

valleys,  often 

tered  from  the 

ice*bergs,  and 
e  piece  which 
>ur  fathoms ;  it 
id  of  the  same 

account  of  ice- 
hn  Cartwright, 
bligation. — See 

•b.  28,  1776. 
now  send  you, 
ho  hath  resided 
of  those  great 
lumbers  on  the 
y^  called  Islands 

>,  is  frozen  to  a 

prevailing  and 

other  Westerly 

a  the  ice  at  the 

them,  although 

lose  about  Lul- 

having  passed 

the  undisturbed 

e  from  the  land, 

the  frozen  sur- 

irpendicalar,  an 

;he  wind.    The 

lied  with  snow ; 

ite  naked,  are 


Others,  which  happen  to  have  projected  over  the 
sea,  may  have  had  their  foundations  so  sapped  by 
the  waves  during  a  storm,*  as  to  have  lost  their  sup- 
entirely  swept  clear  of  snow  by  the  violence  of  the  storms,  and  what 
would  otherwise  have  Iain  there  is  carried  to  the  leeward  of  the 
hills,  and  under  the  shelter  of  the  cliffs,  where  it  is  deposited  in 
infinitely  greater  quantities  than  it  would  fall  in  without  such  a 
cause.    The  hypothenuse  of  such  triangle  is  frequently  of  such  a 
slope  as  that  a  man  may  walk  up  or  down  without  difficulty.     By 
frequent  thaws,  and  the  occasional  fall  of  moisture  interrupting  the 
frost,  during  the  first  parts  of  the  winter,  the  snow  will,  in  some  small 
degree,  dissolve,  by  which  means  it  only  acquires  a  greater  hardness 
when  the  frost  returns  ;  and  during  the  course  of  that  rigorous  sea- 
son it  generally  becomes  a  very  compact  body  of  snow  ice.     In  the 
spring  of  the  year  the  icy  base  gives  way,  and  its  burden  plunges 
into  the  sea,  sometimes  entire,  sometimes  in  many  fragments.     As 
the  depth  of  water  in  many  parts  is  forty,  fifty,  one  hundred  fathoms, 
and  upwards,  close  to  the  shore,  these  bodies  of  ice,  vast  as  is  their 
bulk,  will  frequently  float  without  any  diminution  of  their  contents, 
although  the  very  large  ones  do  often  take  the  ground,  and  sometimes 
are  not  sufficiently  reduced  by  either  the  penetration  of  the  sea  and 
the  rain  water,  or  of  a  whole  summer's  sun,  to  get  at  liberty  again 
before  another  winter.  •  "^ 

;  "  The  above  relation,  which  my  brother  gives  from  his  own  ob- 
■ervation,  in  North  latitude  52°  15',  accounts  very  naturally  and 
easily  for  the  formation  of  that  surprising  number  of  the  vast  pieces 
of  ice  which  is  annually  seen  on  the  Labrador  coast,  and  considerably 
to  the  Southward.  .',;.' 

"  Jonk  Cartwrioht." 

*  "  The  sea  has  washed  underneath  the  ice  cliffs,  as  high  as  the 
Kentish  Forelands,  and  the  arches  overhanging,  support  mountains 
of  snow,  which  have  lain  since  the  creation." — ^Wood's  Voyage, 

p.  20.  -  ■\-  ■■  -;v'-. .  ■ '..  '■    .:    ■'  '■■  :  ■ 

"  Cuncta  gelu,  canaque  ^ternJUh)  ^hdine  tecta,    ^f     ..  \ 
Atque  aevi  glaciem  cohibent,  riget  ardua  mentis  *   '      '''* 
iEtherii  facies,  surgentique  obvia  Phcebo, 
'  Dnratas  nescit  flammis  mollire  pruinas." 

Silius  Italicus,  lib.  iii.  I.  480. 


/ 


t     1 


■f 


;#•■' 


v* 


%• 


Idd 


pK  APP110ACHIN9 


^ 


t*f- 


\ 


K- 


port ;  whilst  others  again  may  have  been  red  from 
the  mass  to  which  they  before  adliered  by  the  expan- 
sive power  of  the  frost.  • 

,  Great  part  of  the  field,  or  lower  ice,  I  take  to  be 
formed  by  the  sdow  falling  on  the  sands  left  bare  for 
Bix  hours  (from  half  ebb  to  half  flood)  which  imme- 
diately dissolves  upon  touching  the  sands,  and,  before 
the  tide  returns,  becomes  solid  ice ;  part  of  these 
pieces  are  by  the  wind,  or  tide,  again  returned  to  the 
same  sands,  where  they  again  meet  with  another 
store  of  ice,  formed  during  another  six  hours,  which, 
in  the  course  of  a  winter,  must,  by  packing,  accumu- 
latle  to  immense  masses.  That  this  is  not  mere  con- 
jecture, but  the  fact,  I  appeal  to  Captain  Jameses 
account  of  what  he  himself  was  witness  of  whilst  he 
wintered  at  Charlton  Island,  in  Huflson's  Bay.t 

Now,  if  we  examine  a  globe,  we  shall  find,  that 
from  sixty  to  seventy  degrees  of  Northern  latitude 
more  than  half  its  circumference  is  land,  which  is 
open  to  a  Northern  Sea,  from  which  large  tract  of 
coast  much  greater  quantities  of  floating  ice  may  be 
derived  than  have  ever  been  met  with  by  navigators, 
without  being  obliged  to  suppose  that  any  part  of  it 
is  formed  from  sea  water.        *=»'■• 

But  it  may  be  said,  that  our  late  enterprising  navi- 
gators to  the  Southward  have  also  met  with  as  great 

*  "  The  rocks  along  the  coast  burst  with  a  report  equal  to  that  of 
artillery,  and  the  splinters  are  thrown  to  an  amazing  distance."  Mr. 
Wales,  in  Philosophical  Transactions,  vol.  Ix.  p.  125. 

t  For  Captain  James's  account,  see  Boyle,  vol.  ii. ;  as  also  Har- 
ris, vol.  ii,  p.  420.  where  it  is  considerably  abridged,  and  differs  in 
some  few  circumstances.  It  is  stated,  however,  that  in  few  hours 
the  snow  thus  frozen  will  be  five  or  six  feet  thick.        ** 


-H.^. 


/    . 


TUB  NORTH  POLB.  r, 


137 


reft  from 
lie  expan* 

ake  to  be 
fl  bare  for 
ich  imme- 
ind,  before 
of  these 
ucd  to  the 
h  another 
irs,  which, 
;,  accumu- 
mere  con- 
in  James's 
'  whilst  he 

1  find,  that 
rn  latitude 
I,  which  is 
^e  tract  of 
ice  may  be 
navigators, 
y  part  of  it 

rising  navi- 
th  as  great 

iqual  to  that  of 
itance."    Mr. 

;  as  also  Har- 
and  differs  in 
:  in  few  hours 


^  quantity  of  ice  in  the  opposite  hemisphere,  without 
scarcely  discovering  any  land.  < 

To  this  I  answer,  that  their  circumnavigation  was, 
at  a  medium,  about  57*  degrees  of  Southern  latitude, 
though  they  made  pushes  greatly  to  the  Southward 
in  three  points,  and  in  one  of  these  to  71'  10'.  In 
the  other  instances,  as  far  as  67*  and  67*  SC. 

There  is  consequently  a  very  large  space  in  which 
there  may  be  many  a  frozen  region,  which  they  have 
not  had  any  opportunity  of  discovering.  If,  for  exam- 
ple, a  navigator  from  the  Southern  was  sent  upon 
discoveries  to  the  Northern  hemisphere,  and  Europe, 
as  well  as  Asia  and  North  America,  having  been  sunk 
by  earthquakes,  was  to  report  that  he  had  circum- 
navigated at  55*  North  latitude  at  a  medium ;  made 
pushes  even  to  71*  in  different  directions,  without 
seeing  any  continent ;  and  that  therefore  there  was 
no  land  to  the  North  of  55*,  his  countrymen  would 
be  much  deceived  by  such  report,  because  Den- 
mark, Norway,  Sweden,  Muscovy,  Tartarian  Asia, 
and  part  of  North  America,  continued  in  their 
present  situation. 

Besides,  however,  the  ice  which  may  come  from 
Terra  del  Fuego,  Captain  Cook  hath  discovered  two 
frozen  islands  between  Cape  Horn  and  that  of  Good 
Hope,  which  were  covered  with  ice   and  snow.* 

*  Hence  whatever  land  is  discovered  to  the  South  of  this  latitude 
must  produce  ice.  There  is  also  a  ittrge  tract  of  hind,  named  in 
Bome  maps  the  Gulf  of  St.  Sebastian,  which  is  not  far  distant  from 
Georgia  Australis,  and  which  possibly  may  have  escaped  CuptiUn 
Cook.  This  great  navigator  also  conceives,  that  the  ire  floats  from 
^0°  South,  and  is  detached  by  accidents  from  land  lying  to  the 


•ff^ 


^ 


158 


ON  APf*ROACHINa 


w 


'   1^^ 


^% 


^. 


v^" 


The  first  of  these,  situate  in  54%  is  called  Georgia 
JimtraUs ;  and  the  second,  Sandmch  Land^  in  59**, 
which  appeared  so  large,  to  some  eyes,  that  it  was 
conceived  to  be  part  of  a  continent.* 

It  is  believed  also,  that  no  ship  hath  been  beyond 
48"*  to  the  Southward  of  New  Zealand ;  and  from  the 
coldness  of  the  most  Southern  of  these  large  islands, 
I  cannot  but  suspect  that  there  is  a  considerable  tract 
of  land  between  it  and  the  Pole. 

Having  thus  endeavoured  to  account  how  the  float- 
ing ice  which  is  met  with  may  be  supposed  to  be 
formed  from  snow  or  fresh  water ;  I  cannot  but  risk 
another  conjecture,  that  the  time  of  the  year  at  which 
atte;npts  are  commonly  made  to  make  discoveries 
towards  the  two  Poles  (though  favourable  in  many 
other  circumstancest)  is  probably  the  season  when 
the  greatest  quantity  of  floating  ice  will  be  observed. 

South  of  that  parallel,  as  the  currents  in  the  Antarctic  seas  always  set 
to  the  North. — Cook's  Voyage,  vol.  i.  p.  268. 

Captain  Fumeaux  in  1744,  passed  between  Georgia  Australis  and 
Sandwich  Land  (rather  supposed  a  continent,)  without  seeing  either 
of  these  new  discoveries,  though  the  mountains  on  both  are  remark- 
ably high,  particularly  U^ose  in  Sandwich  Land,  one  of  which,  by 
several,  was  considered  to  equal  Teneriffe. 

Captain  Fumeaux  could  not  have  been  well  more  than  two 
degrees  from  either  of  these  countries. — See  his  Track  in  the  lately 
published  map.  '  :••./-- 

*  See  Captain  Cook's  Voyage,  vol.  ii.  p.  230 ;  where  he  supposes 
land  near  the  South  Pole,  chiefly  opposite  to  the  Southern  Atlantic, 
and  Indian  Oceans,  as  on  those  meridians  ice  is  found  as  far  North  as 
48".  It  is  in  this  tract  of  Southern  land  that  Cook  supposes  the  ice  to 
be  chiefly  formed,  which  is  met  with  in  the  Southern  Oceans. — Ibid. 

t  Viz.  The  nights  being  shorter,  and  the  rigging  not  being 
so  subject  to  being  frozen. 


%" 
* 


iif^- 


* 


1^ 


M 


THE  NORTH  POLE. 


0 


159 


J  This  seems  to  follow  as  a  necessary  consequence 
from  the  push  being  never  made  before  midsummer, 
and  often  a  month  later,  which  is  precisely  the  time 
when  the  ice  begins  to  break  up  in  the  fresh  water 
rivers,  &c. 

I  have  accordingly  minuted  down,  from  several 
voyiiges  in  high  Northern  latitudes,  the  day  on  which 
the  navigators  first  mention  seeing  the  floating  ice. 

The  result  of  which  is  as  follows : — 

*    .r  I  ■       ■      ■  . 

Sir  Martin  Frobisher  on  the  23d  of  June, — ^Hack' 
luyt,  vol.  ii.  p.  77. 

Davis  in  his  first  voyage,  July  19th.  In  his  third, 
July  2d.— Ibid.  p.  99.  ^  v  r .  ^ 

Pet  and  Jackman  on  the  13th  of  July. — ^Ibid.  p. 
447. 

Burrow  on  the  21st  of  July. — ^Ibid.  p.  277. 

Governor  Ellis,  July  5th. — ^Voyage  to  discover  the 
Northwest  passage,  p.  127. 

"The  shores  of  Hudson's  Bay  have  many  inlets  or 
friths,  which  are  full  of  ice  and  snow,  and  frozen  to 
the  ground.  These  are  broke  loose,  and  launched 
into  the  sea,  by  land  floods,  during  the  months  of 
June,  July,  and  August." — Ibid. 

"  The  first  floating  ice,  which  is  observed  on  the 
coast  of  Labrador  is  a  joyful  presage  to  the  inhabit- 
ants of  the  approach  of  summer." — Lieutenant  Cur- 
tis, in  Philosophical  Transactions.  .  -•    , 

"The  ice  begins  to  break  up  the  18th  of  June." — 
Danish  account  of  Greenland. — Voyages  auJVordy  vol. 

i.  p.  167.  :'■  ■■■■.'■■-^■^-      •■        •      ^'    :■■;■-'  -^       ■.        .;      - 


r 

( 

1 


•  4 


I    i 


3!* 


)*•. 


i    • 

I. 


t 


■# 


160 


^^'i'     I  6V  APl>R0ACHl5tf 


^  The  lakes  of  Lapland  continue  frozen  on  June 
the  24th." — Linschoten^s  Voyage,  ibid.  vol.  iv. 

^  On  the  5th  of  Julj,  the  sea  on  two  sides  is  ob- 
served to  be  covered  with  ice." — Ibid.  p.  187.  .^ 

Wood  sees  the  first  ice  in  North  latitude  75"  59',  on 
June  22. 

On  the  17th  of  August  vast  pieces  of  floating  icp.—- 
Ibid. 

"  In  the  month  of  August  th6  French  observe,  on 
the  Labrador  coasts,  mountains  of  ice  as  high  as  the 
ships." — Boyle's  Works,  vol.  ii.  p.  303. 

"On  June  16th,  a  river  in  Hudson's  Bay  breaks 
up." — Mr.  Wale?,  in  Philosophical  Transactions, 
vol.  Ix.  p.  126. 

"  The  mouth  of  the  Lena  is  not  open  till  the  middle 
of  August." — Observations  Geographiques,  par  M.  Engel^ 
p.  229.      /.'■  i,.  •  ,'>^>    V  _ , , .  ^-<>j.  :W,v  ;.j.-i  :^     . 


0 


i. 

k 


With  regard  to  the  ice  which  may  be  observed  irt 
Southern  latitudes,  I  shall  only  take  notice,  that  Sir 
Francis  Drake,  Feuillee,  and  Clipperton,  passed 
Cape  Horn,  or  the  Straits  of  Magellan,  during  the 
month  of  December,  without  mentioning  ice,*  froni 
which  it  should  seem  that  it  breaks  up  chiefly  during 
the  months  of  January,  February,  and  March,  answer- 
ing to  our  July,  August,  and  September.! 

*  See  Callander's  Voyages  under  these  thrfle  articles. 

t  It  may  possibly  break  up  in  some  years  earlier,  perhaps  in 
December ;  but  some  time  must  be  allowed  for  its  floating  to  the 
North,  as  far  as  the  latitude  of  Terra  del  Fuego.    From  the  instaaces 


# 
p.  811 


■"  ^  '^ 


■,:>' 


on  June 

^ 

es  is  oIh 

5' 59,  on 

ngicp^ 

serve,  on 
:h  as  the 

4^y ', .. 

y  breaks 
isactions, 

le  middle 
VI.  Engely 


)served  in 
t,  that  Sir 
I,  passed 
uring  the 
ce,*  fromi 
dj  during 
I,  answer- 


THE   NORTH   POLE. 


161 


Three  Dutch  ships,  which  sailed  on  discoveries 
with  Commodore  Roggewein,  1721,  met  with  much 
ice  to  the  South  of  Cape  Horn  in  the  middle  of 
January.  The  Author  of  the  Narrative  afterward 
makes  this  obse  'ation:  "  Those' mountains  of  ice, 
which  are  seen  in  the  latitude  of  Cape  Horn,  prove 
that  there  is  land  towards  the  Southern  Pole,  it 
being  certain  that  this  ice  cannot  be  formed  in  the 
ocean,  though  the  cold  is  so  severe."* 

But  it  may,  perhaps,  be  said,  that  the  ice  which 
breaks  up  in  June,  July,  and  August,  or  during  the 
correspondent  months  in,  the  opposite  hemisphere, 
may  remain  floating  for  years  without  being  much 
dissolved. 

To  this  I  will  not  take  upon  myself  to  say  that 
some  such  islands,  when  very  large,  may  not  con- 
tinue more  than  a  year;  but  I  should  conceive  this 
not  to  be  very  common.  Storms  and  other  accidents 
must  probably  break  them  into  small  musses  which 
will  quickly  be  thawed ;  as  that  able  geographer  and 
promoter  of  discoveries,  Mr.  Bailiff  Engel,  observes, 
that  if  a  piece  of  ice  is  fastened  by  a  cord  and  let 
down  into  the  sea,  it  is  presently  melted.f 

Mr.  Wales  also  informs  us,  that  he  supposes  most 
of  these  islands  of  ice  are  soon  wasted,  in  the  follow- 


# 


.■•(i 


perhaps  in 
ating  to  the 
he  instaaces 


cited,  it  appears  that  the  earhest  floating  ice  which  is  seen  in  the 
Northern  hemisphere  is  not  observed  sooner  than  the  16th  of  June, 
whilst  in  much  the  greater  part  mention  is  not  made  of  it  till  July. 

*  Histoire  de  V Expedition  ietrois  Vaisseaux,  Sfc.  Hague,   !739. 
p.  81. 

t  See  Obiervationi  Geographiques,  p.  224.  ' 
21 


0 


■^'- 


VJ 


,♦ 


W: 


162 


ON  APPROACHINCi 


■*^'- 


-   ^■ 


ing  words :  '^  The  truth  is,  their  motion  and  dissolu- 
tion are  apparently  so  very  quick,  that  I  am  of  opin- 
ion it  must  be  a  pretty  large  island  which  is  not 
dissolved  in  one  summer."* 

How  soon  likewise  does  the  ice  disappear,  which 
is  discharged  from  our  own  rivers  into  the  sea,  after 
our  most  intense  frosts  ?  v>   ••* 

1  have  omitted  stating  the  degree  of  cold  at  which 
the  sea  water  I  exposed  to  the  air  began  to  be  frozen, 
and  cannot  now  recover  the  memorandum  which  I 
made  at  the  time.  I  am  pretty  confident,  however, 
that  the  mercury  had  sunk  only  to  twenty-seven. 

But  though  congelation  thus  took  place  at  five 
degrees  below  the  freezing  point,  it  is  proper  that 
I  should  state  some  other  circumstances  attending 
the  experiment. 

The  sea  water  which  I  used  came  from  the  North 
Foreland,  which  is  at  the  mouth  of  the  Thames,  and 
consequently,  not  being  the  same  with  that  of  the 
ocean,  was  more  easily  frozen. 

Besides  this,  the  quantity  was  so  small  as  not  to 
cover  a  thin  china  bason  deeper  than  an  inch,  both 
which  particulars  contribute  greatly  to  the  more 
speedy  formation  of  ice ;  it  need  scarcely  be  men- 
tioned also,  that  the  li  juid  to  be  frozen  v«^as  in  a 
quiescent  state. 

How  much  a  considerable  degree  of  motion  im- 
pedes congelation,  may  be  inferred  from  what  may 
be  observed  in  every  river;  for  as  high  as  the  tide 
hath  any  force,  I  doubt  much  whether  any  ice  is 


*  Philosophical  Transactions,  vol.  Ix.  p.  112. 


m* 


■i^ 


dissolu- 

of  opin- 

2h  is  not 

ir,  which 
^ea,  after 

at  which 

e  frozen, 
which  I 

however, 
even, 
se  at  five 
•oper  that 

attending 

the  North 
ames,  and 
hat  of  the 

as  not  to 
inch,  hoth 

the  more 
f  be  men- 

v/as  in  a 

notion  im- 
what  may 
ls  the  tide 
my  ice  is 


y    ,^ 


'T* 


V* 


■<>W^' 


THE  NORTH  POLE. 


16'3 


acarcely  ever  formed  in  the  fair  open  channel,  during 
our  most  intense  frosts.  1  attended  to  the  Thames, 
in  this  respect,  during  the  late  severity  of  the  weather, 
and  it  seemed  to  me  that  all  the  ice  floated  down 
from  the  upper  parts  of  the  river ;  but  packing  after- 
ward between  the  lighters,  occasioned  the  formation 
of  very  large  masses. 

I  have  little  doubt,  from  these  circumstances,  but 
that  the  open  sea,  if  it  be  frozen  at  all,  must  require 
a  much  more  intense  cold  than  twenty-seven ;  allow- 
ing however  any  greater  degree  of  cold  in  the  high 
latitudes,  it  seems  deducible,  from  the  experiments 
of  Dr.  Higgins,  that  sea  water  cannot  be  frozen  into 
a  solid  state,  if  compared  with  that  of  ice  formed 
from  the  water  of  rivers;  nor  will  such  ice  when 
melted  become  palatable,  unless  it  hath  been  pre- 
viously washed  in  fresh  water. 

Hence  it  seems  almost  to  be  demonstration,  that 
the  floating  ice  met  with  by  navigators,  being  both 
solid  and  sweet  to  the  taste  after  dissolution,  cannot 
be  produced  from  the  water  of  the  ocean.* 

I  will  venture  also  to  insist,  that  if  such  ice  was 
actually  frozen  from  the  ocean,  it  must  very  quickly 
be  melted,  because,  as  it  must  consist  of  detached 
laminse  intercepting  the  brine,  the  sea  would  soon 
insinuate  itself  between  the  interstices,  so  as  to  cause 
its  dissolution.  If  any  ice,  therefore,  should  be  form- 
ed in  those  parts  of  bays  which  are  land  locked, 

*  The  ice  taken  up  by  Cuptain  Cook,  during  his  circumnavigation 
in  high  Southern  latitudes,  was  sohd  and  transparent :  being  placed 
idso  on  the  deck  for  the  salt  water  to  drain  off,  the  ice  became  whole- 
•iomo  and  palatable  water. 


;■»■ 


^ 


m. 


■*f. 


164 


ON  APPROACHING  THE  NORTH  POLE. 


^ 


have,  little  or  no  tide,  and  receive  con8iderab)«; 
quantities  of  fresh  water,  when  such  ice  is  wafted 
fairlj  out  to  sea,  I  should  conceive  that  it  must  dis- 
appear in  a  very  short  time.  .        ,        ,^. 


♦ 


O.'C 


.A 


■Sfi. 


i,    ',•*,■  ^ 


.^'-f^. 


•  M  ■ 


^ 


•»' 


APPENDIX. 


>'' 


J-  "s  1- 
t  ' 


PAPEH8 

APPROACHINQ  THE  NORTH  POLE 

AND  ON 

A  NORTHWEST  PASSAGE. 


#1 


COLONEL  BEAUFOY,  F.R.S. 


The  Papers  are  extracted  from  Thonuon's  Annals  of  niilosophj,  by  pemiissiou 
ef  Colonel  Bcaufov. 


* 


i 


W-    'f  ' 


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w^ 


'■si?: 


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■fi    V 


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1  \ 


M: 


-,'     ?■-•■ 


.  1 


»     -  ,T 
■      5. 


«  . 


A;.^ 


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<    '  •     ,'  ^     ■  -    ■  -    -  ■  >^  .■  . 


~  t 


M 


'.■'"(ti^;     -^ii-.  ■•*;- 


■?-> 


APPENDIX. 


A,  V      QUERIES 

r  ■  REIPEGTINO 

THE   FRODABILITT    OF   REACHING, 

FROM 

The  Island  of  Spitzbergen,  the  ^orth  Pole, 


.) 


*;,,v'^^   ^ 


BY  MBANI  OF 

REIX-DEER,  DURING  THE  WINTER  ; 

'  —:      -•>';    •'  AND 

'■;;_•■       .■\^'     ANSWERED    fV -.r^-^v.  • ,-.;-  . 


PERSOJ^S  WHO  WIJ^TEBED  THERE. 


Some  years  past  I  was  impressed  with  the  idea  of 
the  possibility  of  reaching  the  North  Pole  from  Spitz- 
bergen,  during  the  winter,  by  travelling  over  the  ice 
and  snow  in  sledges  drawn  by  rein-deer.  There- 
fore, with  the  view  of  determining  how  far  this  plan 
was  practicable,  I  sent  several  Queries,  and  re- 
quested Answers  to  them  from  Russians,  who  were 
at  that  time  living  at  Archangel,  and  had  wintered 
in  those  remote  islands.  Those  Queries,  together 
wit.  the  Answers,  are  as  follow,  as  I  leani  from  con- 


\i 


•t  i. 


^,     i^ 


i    *  V 


% 


168 


ON  APPROACHING 


« 


i 


I) 


:,tf. 


versation  that  the  practicability  of  such  a  journey, 
conducted  in  a  similar  manner,  is  entertained  by 
well-informed  persons ;  and,  before  a  plan  is  put  in 
execution,  it  is  desirable  to  know  what  has  been 
previously  done  on  the  same  subject.  The  31st  and 
33d  seem  contradictory,  probably  from  some  error  in 
translating  the  Questions  into  Russ,  or  the  Answcrn 
into  English.       ' 

-  ''        ''  • 

1.  Query.  How  many  settlements  have  the  Rus- 
sians on  the  island  of  Spitzbergen,  and  which  is  the 
most  Northerly  ? 

^  Answer.  There  are  neither  settlements  nor  fixed 
inhabitants  in  Spitzbergen,  except  those  fishermen 
who  go  there  in  quest  of  fish,  and  likewise  of  those 
animals  from  Megen,  Archangel,  Onega,  Rala,  and 
other  places  bordering  the  White  Sea,  in  vessels 
from  sixty  to  one  hundred  and  sixty  tons.  They  sail 
from  the  above-mentioned  places,  those  for  the  sum- 
mer fishery  in  the  beginning  of  June,  and  those  for 
the  winter  in  June  and  July.  They  arrive  on  the 
West  side  of  Spitzbergen,  and  commonly  return 
home,  the  former  some  year  in  September,  and  the 
latter  the  next  year  in  August  and  September.  They 
winter  in  the  Gulfs  of  Devil  Bay,  Clock  Bay,  Ring 
Bay,  Crus  Bay,  German  Island,  Magdalene  Bay,  and 
to  the  Northward  in  Liefde  Bay,  and  others.  The 
farthest  North  our  fishermen  ever  have  sailed  to  is 
Liefde  Bay,  and  from  thence  in  small  boats  as  far 
as  Nordoster  Island. 

2.  Q.  At  what  time  of  the  year  does  the  winter 
commence? 


Idk- 


f    - 


■»  Jl » ;  «^.^  «^^|.« 


THE  NORTH  POLE. 


169 


journey, 
ined  by 
is  put  in 
as  been 
31st  and 
error  in 
Answers 


the  Rus- 
ch  is  the 

nor  fixed 
ishermen 

of  those 
iala,  and 
1  vessels 
rhey  sail 
the  sum- 
those  for 
e  on  the 
\y  return 

and  the 
T.  They 
ay,  Ring 
Bay,  and 
rs.  The 
led  to  is 
ts  as  far 

le  winter 


A.  The  winter  generally  sets  In  about  the  latter 
end  of  September  and  beginning  of  October. 

3.  Q.  Is  it  ushered  in  by  storms  ?  and  is  any  one 
wind  particularly  productive  of  them  ? 

J.  A.  The  winter  sometimes  sets  in  with  winds  from 
the  North,  North  Northwest,  and  Northwest;  and 
sometimes  commences  with  calm  weather,  hard  frosts 
accompanied  with  snow. 

4.  Q.  Is  the  weather,  generally  speaking,  calm  in 
winter,  or  are  the  winds  high  ? 

A.  The  winds  are  very  high  and  frequent;  so 
that  two-tliirds  of  the  winter  may  be  said  to  be 
boisterous. 

5.  Q.  What  quantity  of  snow  do  you  suppose  falls 
annually ;  that  is,  to  what  depth  on  the  ground  ? 

A.  On  even  places  the  snow  is  from  three  to  five 
feet  deep ;  but  the  winds  drive  it  from  place  to  place, 
so  as  sometimes  to  render  all  paesage  impracticable ; 
and  on  the  coasts  between  the  hills  there  are  moun- 
tains of  ice,  occasioned  by  the  pressure  of  the  waters 
and  drift  of  snow. 

6.  Q.  Are  the  storms  of  snow  frequent,  and  of 
long  duration? 

A.  The  storms  of  snow  are  very  frequent,  con- 
tinuing for  two,  three,  and  four  days,  and  sometimes 
for  as  many  weeks;  but  the  latter  do  not  occur 
above  once  or  twice  in  a  year.  •-  ^i-    ' 

7.  Q.  Is  the  cold  much  more  severe  at  Spitzber- 
gen  than  at  Archangel  ?  Has  the  degree  ever  been 
ascertained  by  the  thermometer.^  If  it  has,  what 
was  it?        -•  ■•;,  .V  v(-*i:>,vf^i  ^>-->v-. '^>V  •^-J'^^'l-^^y^if- 


^ 


.:0 


Al> 


ON  APPnOACHINU 


A.  From  the  fishennen^s  remarks,  the  cold  is 
more  severe  at  Spitzbergen  than  at  Archangel ;  but 
the  degree  is  not  known,  as  the  people  who  go  there 
have  no  thermometers. 

8.  Q.  Is  the  cold  ever  so  intense  as.  to.  render 
going  abroad  dangerous?  '  -*■  ■-     ' - 

A.  The  cold  is  never  so  severe  as  to  hinder 
the  fishermen,  they  being  accustomed  to  it,  from 
exposing  themselves ;  but  sometimes  the  winds  and 
drifts  of  snow  confine  them  to  their  huts.      .>:..  "<riui«'.' 

9.  Q.  Admitting  it  to  be  so,  by  what  exercise  do 
the  Russians  keep  ofi'the  scurvy  ?  .  i.  </:^' 

A.  When  the  last-mentioned  weather  is  an  obt 
atacle  to  their  leaving  their  huts,  they  keep  off  the 
scurvy  by  the  exercise  of  throwing  the  snow  from  off 
and  around  their  huts,  which  from  stormy  weather 
are  often  buried ;  and  in  order  to  get  out,  they  are 
then  obliged  to  make  a  passage  through  the  roof. 
They  likewise  oppose  the  distemper  by  making  use 
of  a  particular  sallad  or  herb,  which  grows  there  on 
stones,  and  with  which  they  generally  provide  them-, 
selves  in  due  time  against  winter;  but  sometimes, 
from  necessity,  they  are  obliged  to  dig  through  the 
snow  for  it.  Some  of  it  they  eat  without  any  pre- 
paration; and  a  part  they  scald  with  water,  and 
drink  the  liquid.  They  also  carry  with  them  for  the 
same  purpose,  as  a  preventative,  a  raspberry,  called 
in  Russia  moroshka^  which  they  preserve  by. baking 
with  rye  flour,  which  they  eat ;  and  when  pressed, 
drink  the  juice.  They  also  take  fir  tops  with  them, 
which  they  boil;  and  the  water  they  drink  as  an 
antidote,  likewise  against  the  scurvy. 


•mi 


THE  NORTH  ^OLB. 


f 

171 


10.  Q.    In  what  manner  are  the  huts  constructed  ? 
A.    The  huts  the  people  use,  they  always  take 

with  them  in  their  vessels,  and  on  their  arrival  there 
put  them  together.  They  are  constructed  of  thin 
boards,  and  in  the  same  manner  as  the  peasants* 
houses  here.  They  likewise  generally  take  brick* 
with  them  for  building  their  stoves ;  but  when  they  fall 
short,  clay  found  there  is  made  use  of  in  their  stead. 
Their  largest  hut,  which  is  erected  in  the  ncighbout- 
hood  of  their  vc^isels,  boats,  &c.,  is  [torn  twenty  to 
twenty-five  feet  square,  and  serves  as  a  station  and 
magazine ;  but  those  huts  the  men  erect  who  go  in 
quest  of  skins  are  only  from  seven  to  eight  feet 
square,  and  in  the  autumn  are  carried  along  the 
shores  in  boats,  and  put  up  at  distances  from  each 
other  of  ten  to  fitly  Russian  versts.  They  take  the 
necessary  provisions  with  them  for  the  whole  winter 
to  serve  two  or  three  men,  as  many  generally  occupy- 
ing each  hut.  ^" 

11.  Q.  What  fuel  have  they,  and  in  what  manner 
are  their  huts  heated  ?      •    ■   --  •* 

A.  The  fuel  commonly  used  for  hieating  their  hut's 
is  wood,  which  they  likewise  bring  with  them  in  their 
vessels,  and  land  at  the  station  hut.  In  autumn  the 
necessary  quantity  for  heating  the  aforesaid  small 
huts  is  conveyed  in  boats,  or  on  small  hand  sledges, 
to  the  destined  places.  They  often  meet  with  wood 
there  too,  thrown  by  the  sea  on  the  shores. 

12.  Q.  On  what  kinds  of  provisions  do  the  Rus- 
sians subsist  during  the  winter  ? 

A.  The  provisions  they  subsist  on  during  the  win- 
ter consist  in  rye  flour  (of  which  they  make  bread,) 


1^- 


"^ 


»■ 


IP.*    ^; 


v.. 


1^ 


^ 


#  . 


-f 

172 


'0 


V 


•N  APPROACHING 


salt  beef,  ealt  cod,  and  salted  halibut,  butter,  oat 
and  barley  meal,  curdled  milk,  peas,  honey,  linseed 
oil ;  all  which  they  bring  to  Spitzbergen  with  them, 
and  divide  the  same  proportionably  by  weight  to 
each  man.  Their  employers  allow  them  provisions 
for  one  year  and  a  half,  besides  which  the  fishermen 
kill  wild-lion  deer  in  winter,  and  birds  in  summer, 
which  are  experienced  to  be  excellent  food,  and  very 
healthy. 

13.  Q.  Do  they  chiefly  use  spirituous  or  malt 
liquors.^      -.■-,■..  ...,.m  ■.        .,.,     .»■.:.•-■  i-^i^iifet-  -^ 

A.  They  chiefly  drink  a  liquor  called  nuas^  made 
from  rye  flour  and  water.  Malt  and  spirituous 
liquors  are  entirely  excluded  and  forbidden  by  their 
employers,  to  prevent  drunkenness,  as  the  Russians, 
when  they  had  it,  drank  so  immoderately  that  work 
was  often  neglected  entirely. 

14.  Q.  When  in  tlie  open  air,  how  do  they  defend 
themselves  ? 

A.  They  defend  themselves  from  the  rigour  of  the 
weather  by  a  covering  made  of  skin,  above  which 
they  wear  another  made  of  the  skin  of  rein-deer, 
called  kushy^  and  wear  boots  of  the  same. 

15.  Q.  Do  they  not  use  masks,  and  omit  the  prac- 
tice of  shaving  .^  1   .       - --.'■'- 

A.  They  use  no  masks,  nor  do  they  shave ;  but  they 
wear  a  large  warm  cap,  called  tmechy,  which  covers 
the  whole  head  and  neck,  and  most  part  of  the  face. 
They  also  wear  gloves. of  sheep-skin.  ^^  •.• 

16.  Q.  Do  the  inhabitants  cross  the  country  dur- 
ing the  winter?       ;  ^.      „    .  -    .      ; ,   . 


.'■  ii;'«(7r  j    :j    ',':, 


^\ 


^. 


la 


THE  NORTH  POLE. 


173 


utter,  oat 
y,  linseed 
vith  them, 
weight  to 
provisions 
fishermen 
1  summer, 
,  and  very 

i  or  malt 

uas^  made 
spirituous 
n  by  their 
Russians, 
hat  work 

ey  defend 

our  of the 
ve  which 
•ein-deer, 

the  prac- 

but  they 

:h  covers 

the  face. 

ntry  dur- 


A.  There  are  no  inhabitants,  'as  said  before ;  but 
the  fishermen  who  are  there  for  a  time,  do  go  over 
firom  one  island  to  the  other  of  small  distances. 

17.  Q.  How  do  they  travel,  at  what  rate,  and  how 
carry  the  necessary  stock  of  provisions  for  their  sub- 
sistence during  the  journey  ? 

A.  They  travel  on  foot ;  that  is,  on  snow  skaits, 
and  draw  their  food  after  them  in  small  hand  sledges ; 
but  those  who  bring  dogs  with  them  make  use  of  the 
same.  When  travelling,  snow  is  their  drink.  Horses 
or  rein-deer  would  be  of  no  use  to  them  for  the  con- 
veyance of  their  provisions ;  nor  have  they  any. 

18.  Q.  By  what  means  do  they  procure  w^ater; 
and  is  it  by  melting  snow,  or  do  they  find  springs  ?   ^ 

A.  They  use  spring  water  when  it  is  to  be  had, 
often  take  it  from  lakes,  and  from  necessity,  some- 
times dissolve  snow ;  but  it  seldpm  happens  that  they 
are  in  want  of  fresh  water,  because  they  commonly 
pitch  on  those  places  w^here  it  is  to  be  met  with. 

19.  Q.  Is  not  the  ice  so  firmly  consolidated  as  to 
render  all  passage  across  it  from  one  island  to  the 
other  perfectly  safe  during  winter  ? 

A.  The  ice  at  Spitzbergen  is  well  consolidated ; 
and  in  some  places  the  flakes  run  to  a  great  height, 
one  on  another,  which  makes  even  the  passage  on 
foot  very  difficult;  other  places  are  quite  smooth, 
except  those  gulfs  which  run  into  the  land  about 
twenty  versts,  where  the  ice  is  continually  floating 
and  drifting ;  but  travelling  with  horses  or  rein-deer 
is  quite  impossible. 

20.  Q.  Is  not  the  ice  rendered  smooth  by  the 
interstices  being  filled  up  with  snow  ? 


■i* 


V 


ir: 


*  ,.;  '5^ 


Mi 


174 


ON  APPROACHING 


-m 


t 


A.  As  before  said,  the  ice  is  made  smooth  by  the 
Bnow  filling  up  the  inequalities.       /     ■ 

21.  Q.  Does  any  danger  arise  either  in  crossing 
tLe  land  or  the  ice,  from  the  drifting  of  the  snow  } 

A.  They  do  not  journey  in  winter,  as  beforemen- 
tioned,  except  to  islands  at  trifling  distances ;  and  a 
traveller  is  in  much  danger  if  surprised  by  a  sudden 
gale  of  wind,  accompanied  by  drifts  of  snow ;  he  ia 

obliged  to  lie  down,  covering  himself  with  his <, 

and  remain  so  secured  till  the  hurricane  is  over ;  but 
when  it  continues  for  any  length  of  time,  th^  poor 
wretch  often  perishes. 

22.  Q.     What  degree  of  light  is  there  in  winter  ? 
A.    The  fishermen  do  not  know  what  the  degree 

of  light  may  be  in  winter;  indeed,  they  are  ignorant  o*' 
the  meaning  of  the  term :  however,  they  say  that  from 
the  latter  end  of  October  to  the  12th  of  January  the 
sun  does  not  appear  above  the  horizon,  which  causes 
a  continual  darkness,  and  obliges  them  always  to 
keep  a  light  in  their  huts  by  burning  train  oil  in 
lamps ;  but  as  soon  as  the  sun  makes  its  appearance, 
the  days  increase  very  rapidly. 

23.  Q.  What  difference  does  the  absence  of  the 
moon  occasion  ?  Are  the  stars  in  general  brilliant  ? 
Can  you  see  to  read  when  the  moon  is  under  the 
horizon  ? 

A.  From  the  appearance  of  the  moon  in  her 
second  quarter  to  her  decline  in  the  last,  the  nights 
are  very  luminous,  and  the  stars  f  xtraordinarily  light 
both  day  and  night.  In  the  gloom  of  winter  the  peo- 
ple keep  time  from  the  position  of  certain  stars. 


i* 


V* 


^. 


f . 


V:?'' 


THE  NORTH  FOLK. 


# 


175 


When  the  moon  is  below  the  horizon,  it  is  impoBsible 
to  read. 

24.  Q.  Is  the  Aurora  Borealis  very  brilliant ;  and 
in  what  part  of  the  horizon  is  it  seen  ? 

A.  In  the  dark  time  of  winter  the  Aurora  Borealis 
in  commonly  seen  most  strong  in  the  Norih,  and  ap- 
pears very  red  and  fiery. 

25.  Q.  Does  it  appear  possible  to  cross  the  ice 
in  winter  to  the  North  Pole  .'*  If  it  does  not,  what 
are  the  obstacles  ?  '  ' 

A.  The  likelihood  of  a  passage  to  the  North  Pole 
does  not  seem  probable  to  the  fishermen,  as  they 
have  not  had  an  opportunity  to  attempt  it ;  and,  from 
their  observations,  think  all  passage  impossible,  as 
the  mountains  of  ice  appear  monstrously  large  and 
lofty.  Some  of  the  ice  is  continually  drifting  about ; 
so  that  in  many  places  water  is  discerned.  Those 
who  have  been  on  the  most  elevated  parts  of  Nord- 
oster  Island  declare,  that,  as  far  as  it  is  visible, 
open  water  is  only  seen ;  but  to  what  distance  it 
may  continue  so,  it  is  impossible  for  them  to  ascer- 
tain, as  an  attempt  for  the  discovery  has  never 
been  made ;  but  seemingly  it  is  practicable  to  bring 
the  fuel  and  provisions  in  vessels  to  the  Nordoster 
island. 

26.  Q.  If  the  passage  should  be  deemed  practi- 
cable, in  what  manner  should  it  be  attempted ;  and 
what  means  of  conveying  fuel  and  provisions  appear 
to  be  the  best  ? 

A.  As  the  fishermen  think  all  passage  impractica- 
ble, it  is  not  in  their  power  to  give  any  answer  t* 
this  demand. 


^/1 
*1 


v      / 


# 


■.i^-,-^':h«k?;iC^. 


176 


?■ 


ON  APPROACHINtf 


■! 


r 


#"' 


27.  Q.  Might  not  three  different  huts,  constructed 
like  those  in  which  the  people  of  Spitzbergen  live, 
together  with  a  sufficient  quantity  of  provisions  in 
«ach  for  half  a  dozen  of  people,  be  conveyed  on 
sledges,  and  be  letl  at  the  different  distances  of  two 
hundred,  of  four  hundred,  of  six  hundred  miles, 
North  of  Spitzbergen,  as  places  of  deposit  for  the 
assistance  of  those  who  shall  undertake  the  journey? 

A.  Such  huts  might  be  built,  and  placed  on  shore, 
as  said  in  the  tenth  article,  at  a  convenient  distance 
from  their  vessels ;  but  as  for  conveying  them  ready 
built  to  the  distances  proposed  appears  to  the  people 
an  impossibility. 

28.  Q.  What  number  of  persons  and  rein-deer, 
or  of  dogs,  would  be  requisite  for  conveying  the  huts  ? 

A.  From  the  mountams  of  ice  and  great  falls  of 
snow,  neither  dogs  nor  rein-deer  would  be  able  to 
to  draw  loads ;  for  the  fishermen  themselves,  to  be  as 
light  as  possible,  go  '>n  snow  skaits. 

29.  Q.  At  what  price  per  man  for  each  day's 
journey  would  the  people  of  Spitzbergen,  if  they 
think  the  adventure  practicable,  be  likely  to  under- 
take the  conduct  of  the  sledges.?  J     :.  ;    •  ; 

A.  As,  in  the  last  reply,  the  fishermen  show  it  is 
not  convenient  there  to  draw  with  dogs  or  rein-deer, 
therefore  no  price  can  be  said. 

30.  Q.  Are  there  any  persons  in  Archangel  who 
have  formerly  resided  in  Spitzbergen  who  would 
engage  in  the  business  ?  and  are  there  any  who  would 
be  willing,  in  company  with  two  Englishmen,  to 
attempt  on  this  plan  a  passage  to  the  North  Pole  ? 


ji» 


^■^. 


THE  NORTH  POLE. 


177 


A.  As  there  are  not,  nor  ever  were,  any  natives 
of  Spitzbergen,  none  therefore  can  be  resident  in 
Archangel :  however,  many  men  may  be  met  with 
here  who  have  wintered  there;  but  as  they  have 
never  made  an  attempt  to  go  to  the  Pole,  they  cannot 
undertake  the  conduct  of  the  business.  Notwith- 
standing, if  an  Englishman  should  determine  on  the 
endeavour,  some  people  might  be  met  with  who 
would  perhaps,  with  an  English  ship's  company, 
engage  themselves. 

31.  Q.  In  the  spring,  have  flights  of  birds  ever 
been  observed  to  direct  their  course  North  o^  Spitz'- 
bergen  ? 

A.  It  has  been  always  experienced  by  those  who 
have  been  at  the  most  northerly  par ii  of  Spitzbergen, 
that  in  the  spring  a  great  number  of  wild  geese, 
ducks,  and  other  birds,  take  their  flight  farther  North. 

32.  Q.  What  animals  and  birds  have  they  during 
the  summer,  and  what  species  winter  on  the  island  ? 

A.  In  Spitzbergen  they  have  wild  rein-deer,  white 
and  blue  fox«s,  and  white  bears,  which  remain  con- 
tinually on  the  island ;  but  geese,  ducks,  6lc.  are 
only  there  in  summer. 

33.  Q.  Those  which  quit  Spitzbergen  on  the 
approach  of  winter,  in  what  month  do  they  generally 
emigrate,  and  to  what  point  of  the  compass  ? 

A.  All  the  before-mentioned  birds  on  the  ap- 
proach of  winter,  that  is,  in  the  latter  end  of  Sep- 
tember, fly  to  the  Southward,  and  return  again  in  the 
latter  end  of  Aoril. 

A. 

N.  B.  The  31  st  and  33d  Answers  do  not  appa* 
rently  agree. 

23 


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THE  NORTHWEST  PASSAGE  j 


••;      .  i '  '  1*.   .  ■  i 


■•.'"* 


«M9. 


THE  INSULAR  FORM  OF  GREENLAND. 


'.r'n\*' 


— <«fiWV~ 


The  reign  of  his  present  Majesty  will  ever  be 
famous  for  the  encouragement  given  to  science ;  but 
in  no  branch  has  the  King^s  gracious  patronage  been 
more  conspicuous  than  in  the  discoveries  made  by 
difierent  circumnavigators,  especially  by  the  immor- 
tal Cook.  Considering  the  inducement  and  encour- 
agement held  out  by  our  monarch  for  exploring  the 
Northern  Parts  of  the  globe,  and  the  number  of  ships 
annually  fitted  out  from  the  different  ports  of  the 
United  Kingdom  for  Davis^s  Straits,  Baffin's  Bay, 
and  Spitzbergen;  it  may  appear  very  remarkable 
that  no  new  discoveries  are  made,  or  old  verified,  or 
any  voyage  extended  to  a  higher  latitude  than  81** 
North.  The  King's  wish  of  promoting  discoveries  in 
this  part  of  the  world  is  evident  fit)m  Lord  Mul- 
grave's  expedition,  and  more  especially  firom  the  Acts 
of  Parliament  promising  a  reward  of  twenty  thousand 
pounds  to  any  of  his  Majesty's  subjects  who  shall 
tail  through  any  passage  between  the  Atlantic  and 


180 


ON  APPROACH  li\  CI 


Pacific  Oceans  to  the  Northwards  of  latitude  52" 
North,  and  also  from  a  reward  of  five  thousand 
pounds  to  any  British  ship  that  shall  approach  within 
one  degree  of  the  North  Pole.  To  what  cause,  then, 
can  he  attributed  the  indiflference  and  apathy  of  those 
commanders  of  Greenland  ships  who,  having  been 
unsuccessful  in  the  fishery,  might  be  supposed  to  have 
it  in  their  power  to  defray  the  expensed  of  the  outfit 
by  sailing  to  the  West  or  the  North,  with  the  view 
of  claiming  one  of  the  above  rewards  ?  It  cannot  be 
said  with  justice  that  the  masters  of  our  Greenlanders 
are  either  deficient  in  skill,  or  indifferent  to  dis- 
covery; for  among  them,  as  in  other  professions, 
men  are  found  of  superior  talent  and  of  enterprising 
spirits.  The  paradox  will,  however,  be  solved  by 
referring  to  the  subjoined  oath,*  which  effectually 
excludes  every  conscientious  person  from  endeavour- 
ing to  carry  into  execution  the  scientific  views  of  the 
Legislature  in  passing  what  may,  without  impro- 
priety, be  named  the  Discovery  Act,  When  this 
last  Act  -whs  passed,  it  is  probable  the  former  Act 


.'"<'•• 


'-JO^*!'*-' 


^  The  foUoTving  is  a  copy  of  the  oath  taken  by  the  master,  and  also 

by  the  owner,  of  Greenland  ships  :  " Master  of  the  ship  

maketh  oath,  that  it  is  really  and  truly  his  firm  purpose,  and  deter- 
mined resolution,  that  the  said  ship  shall,  as  soon  as  license  shall 
be  granted,  forthwith  proceed  so  manned,  furnished,  and  accoutred, 
on  a  voyage  to  the  Greenland  seas,  or  Davis's  Straits,  or  the  seas 
adjacent,  there  in  the  now  approaching  season  to  use  the  utmost 
endeavours  of  himself  and  his  ship's  company  to  take  whales,  or 
other  creatures  living  in  the  seas,  and  on  no  other  design,  or  view 
of  profit,  in  this  present  voyage,  and  to  import  the  whale  fins,  oil, 

and  blubber  thereof,  into  the  port  of Sworn  at  the  Custom 

"House." 


^■ 


THE  NORTH  POLE, 


181 


tude  52° 
thousand 
ch  within 
Jse,  then, 
"f  of  those 
ing  been 
J  to  have 
he  outfit 
the  view 
annot  be 
nlandera 
t  to  dis- 
)fessions, 
erprising 
)lved  by 
Fectually 
deavour- 
\^  of  the 
t  impro- 
hen  this 
•mer  Act 

!r,  and  also 

ship  

and  deter- 
cense  shall 
accoutred, 
>r  the  seas 
he  utmost 
)vhales,  or 
I,  or  view 
J  lius,  oil, 
16  Custom 


for  promoting  Northern  discoveries  did  not  occur  to 
the  frainers.    I  remember  some  years  past  that  a 
learned  and  scientific  Member  of  the  House  of  Com- 
mons was  fio   much  struck  with  the  discouraging 
eflect  of  the  oath,  that  it  was  his  intention  to  have 
brought  forward  a  clause  enabling  the  masters  of 
Greenland  ships  to  prosecute  discoveries  as  well  as 
to  catch  fish ;  and  it  was  owing  to  accident  that  a 
clause  of  the  above  nature  was  not  introduced.    This 
omission,  however,  it  is  hoped,  may  yet  be  supplied 
at  no  distant  period,  and  Greenland  voyages,  con- 
ducted as  they  are  by  seamen  best  qualified  for  such 
an  undertaking,  be  made  subservient  to  the  exploring 
of  the  Northern  regions. 

It  may  farther  be  observed,  navigating  among  the 
ice  being  in  itself  a  science,  men  regularly  brought 
up  to  the  sailing  and  working  of  ships  in  the  Arctic 
Circles  should  be  selected  for  such  service,  in  pre- 
ference to  those  accustomed  to  navigate  the  more 
temperate  parts  of  the  globe.  It  follows,  therefore, 
that  if  at  any  future  period  it  should  be  the  intention 
of  government  to  promote  Northern  discoveries,  it 
would  be  advisable,  both  for  economy  and  the 
greater  probability  of  success,  to  hire  one  of  the 
Greenland  vessels  and  crew,  sending  on  board  as  - 
many  scientific  and  philosophical  men  as  are  deemed 
requisite.  The  following  statement  was  sent  me 
some  years  past  by  Captain  Brown,  an  able  and 
expert  seaman,  regularlv  brought  up  in  the  whale 
fishery,  who  was  willing  to  undertake  the  exploring 
Baffin's  Bay,  or  endeavouring  to  approach  the  North 
Pole.    He  mentioned,  that,  though  in  Barn's  Bay  he 


'\ 


182 


W  APPROACHIVG 


\ 


* 


had  frequently  run  to  the  Westward,  he  had  never 
got  Bight  of  land  in  that  direction ;  which  implies  the 
Northern  part  of  America  may  be  much  contracted. 
Brown,  unfortunately,  was  killed  at  one  of  tho  Sand- 
wich Islands : —  ,  "^  :  ,. 


.•« 


"  SIR, 


"Jan.  IG,  1789. 


*''  I  shall  begin  fitting  out  the  first  of  next  month 
for  Davis^s  Straits ;  and  should  you  wish  to  explore 
Baffin's  Bay,  I  shall  be  glad  to  have  timely  notice, 
that  I  may  prepare  a  larger  stock  of  provisions,  pro- 
vide presents  for  the  Indians,  and  several  other  arti- 
cles which  will  be  necessary  for  that  voyage.  It  will 
be  proper  for  the  bounty  to  be  paid  by  the  Treasury, 
or  the  Custom  House  Oath  altered;  and  I  think, 
when  you  peruse  the  subjoined  account  of  expenses, 
you  will  net  think  my  requisition  of  five  hundred 
pounds  per  month,  for  two  ships,  extravagant.  I  only 
desire  it  to  be  paid  from  the  time  of  leaving  the 
fishery  in  72"  North  till  we  return  to  Cape  Farewell; 
and  no  payment  to  be  made  unless  it  shall  satisfacto-^ 
rily  appear  the  utmost  has  been  done  to  explore  Baf- 
fin's Bay,  Lancaster  Sound,  &c.  The  expense 
government  would  possibly  incur  would  be  very 
trifling;  but  as  underwriters  will  not  ensure  such 
voyages,  the  owners  should  be  indemnified,  and  the 
value  of  the  ships  ascertained  by  the  surveyor  who 
values  the  transports,  against  the  enemy,  and  other 
extra  risks.  1  have  perused  all  the  Northern  voyages, 
and  shall  perfect  myself  in  lunar  observations. 

(Signed) 

"  WILLIAM  BROWN.' 


'*.•' 


<# 


^■ 


-% 


'  % 


*f. 


THE  NORTH  POLE. 


183 


Ship  Butterwortht  three  hundred  and  ninety-two  Tom,*  Boats,  and 

fortyeight  Men, 
■"-  «  ^  PirMonlh, 

1  Master 5    0  0 

1  Surgeon 3  10  0 

1  Chief  Mate 3  10  0 

1  Carpenter 3  10  0 

1  Carpenter's  Mate 2  10  0 

1  Second  Mute 2  10  0 

1  Bontsw.-iin 2  10  0 

1  Skim-man 2  10  0 

1  Cooper 2  10  0 

7  Harpooners,  at  50s.  each 17  10  0 

1  Cook 2    0  0 

7  Boat  stcercrs,  at  40j.  each     .      '#'      .         .         .  14    0    0 

7  Line  coilers,  at  32s.  Gd.  each         .         ,         .         .117    0 

17  Men,  at  30s.  each , 25  10     O 

48  Men's  wages         .         .         .     ,    ,y      .         .         .     98     7     G 
Men's  provision,  at  30s.  each  .         .         .         .     72    0    0 

Wear  and  tear,  392  tons,  at  bl.  per  ton  .        .         .     98    0    0 

!■      ^  ^  £208     7     « 

<  'abin  allowances,  presents  for  Indians,  extra  hquor,  and  other 
encouragement  for  the  people,  cannot  be  estimated  at  less 
than  31/.  12s.  Gd.  per  month,  making  a  total  of  300/. 

Brig  Lyon  one-third' less  expense. 

As  experiments  are  making  on  the  length  of  the 
pendulum  in  the  Orkneys,  it  is  highly  desirable  that 
scientific  men  be  sent  for  the  same  object  in  one  of 
the  Greenland  ships  to  Spitzbergen;  and  at  the  con- 
clusion of  the  fishery  they  might  return  in  the  same 
vessels.  .  .  . 

*  A  Vessel  ot'  the  above  tonnage  with  a  rising  floor  is  the  best  adapted  for  thii  ser 
vlru,  as  it  liaii  a  sufiicieut  moRieutum  ainoDg  the  loose  ice,  and  is  amily  managed. 


^^1 


..*! 


IMAGE  EVALUATION 
TEST  TARGET  (MT-3) 


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1.0 


1.1 


l^|28     12.5 
H:    1^    12.0 


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1-25  i  1.4 


1.6 


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Photographic 

Sciences 

Corporation 


23  WEST  MAIN  STttEET 

WEBSTER,  N.Y.  14580 

(716)  872-4503 


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ON  API>llOACHIKG 


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Every  Greenland  vessel  should  be  furnished  with 
an  artificial  horizon;  of  which  Uie  first  and  best  is  a 
shallow  cylinder  of  wood  four  inches  diameter  in  the 
clear,  and  three-tenths  and  a  half  deep,  into  which, 
by  means  of  an  ivory  funnel,  is  poured  quicksilver. 
To  prevent  the  mercury  from  being  ruffled  by  the 
wind,  two  glass  planes  are  placed  over  it,  whose 
surfaces  are  parallel,  and  forming  an  angle  with  each 
other  of  90° ;  and  if  this  be  not  sufficient  protection 
when  the  mercury  is  agitated  by  wind,  or  any  heavy 
object  j^assing  near,  a  circular  piece  of  glass  is 
floated  on  the  quicksilver.  The  second  (invented,  I 
believe,  by  the  late  Mr*  Adams,  of  Edmonton)  is  a 
plane  concave  glass  four  inches  in  diameter,  and 
ground  to  a  long  radius.  It  is  fitted  into  a  metallic 
box,  with  its  concave  side  downwards.  This  box, 
when  wanted*  is  nearly  filled  with  spirits,  leaving  a 
bubble ;  and  by  means  of  three  screws,  this  bubble  is 
brought  into  the  centre  of  the  glass.  On  one  side  of 
the  box  is  a  ( mall  thumb  screw,  to  be  taken  out  when 
filling,  that  the  air  may  escape.  This  screw  should 
not  be  made  of  iron,  because  it  will  corrode.  If  this 
instrument  be  well  made,  and  pains  taken  in  the 
levelling,  it  may  be  depended  on  to  two  minutes, 
which  gives  an  error  of  one  minute  of  -altitude. 
Neither  of  these  artificial  horizons  can  be  used  when 
the  altitude  of  the  object  exceeds  67°. 

It  would  be  extremely,  curious  to  ascertain  the 
extent  of  the  variation  of  the  compass  in  Baffin's  Bay. 
Captain  Brown  found  it  to  be  79°  42'  West,  in  lati- 
tude 72°  46'  North ;  (see  the  Annals  of  Philosophy, 
vol.  vii.  p.  14.)  and  there  being  an  increase  from  Cape 


-m 


■W'- 


THE  NORTtt  POLE. 


l«d 


Farewell  to  ^his  latitude,  it  is  not  impOBsible,  that  in 
higher  latitudes  the  augmentation  may  continue,  until 
the  needle  loses  its  polarity;  which  extraordinary 
declination  of  the  compass  (peculiar  to  this  part  of 
the  world)  is  so  remarkable,  that,  were  a  vessel  sent 
for  no  other  purpose  than  of  making  magnetkal  ob- 
servations, both  the  time  and  money  which  might  be 
bestowed  on  the  expedition  would  be  advantageously 
employed  for  the  advancement   of  science.    The 
variation  of  the  compass  in  latitude  70'  17'  North, 
and  longitude  163°  24'  West,  is  30°  28'  East;  and  in 
latitude  70°  38',  and  longitude  54°  14'  West,  is  74** 
West ;  whence  it  appears,  that  in  nearly  the  same 
parallel  of  latitude,  and  'in  a  difference  not  exceed- 
ing  109°   10',  or  about  one  thousand  six  hundred 
and    eighty-five    geographical    miles    of  longitude, 
there  is  a  difference  in  the  variation  amounting  to 
84°  42'.    It  would  also  be  a  desirable  discovery  to 
ascertain  whether  on  going  to  the  Westward  it  would 
be  found  that  the  variation  gradually  decreases  to 
the  point  of  no  variation,  and  afterward  gradually 
increases ;  or  whether  its  return  be  not  by  a  sudden 
jump  from  West  to  East.    Observations  on  points  of 
this  description,  accompanied  with  remarks  on  the 
depth,  temperature,  and  saltness  of  the  sea,  and  with 
a  meteorological  journal,  would  contain  much  in- 
teresting and  valuable  information,  and  throw  great 
light  on  the  natural  phenomena  of  these  unexplored 
regions.        '■.  ^   .•!-•■  ^  ■;■■         '••>'  -•    -  :-^ ''■■'-; '\- 

The  depth  of  the  sea  in  Baffin's  Bay  has  been 
determined  beyond  doubt  by  Brown  to  be  more  than 
a  mile.     It  is  not  unusual  in  April   (the  time  the 

21 


•# 


* 


ft" 


»86 


ON  AJ^PROACHING 


^ 


*■        * 


Greenland  fp^els  arrive  in  Daviess  Straits)  for  Fah- 
renheit's Ihermometer  to  stand  at  10°  or  22**  below 
freezing. 

Considerable  diversity  of  opinion  prevails  respect- 
ing the  form  of  Greenland,  which  is  conjectured  by 
some  tp  bend  to  the  Westward,  and,  joining  the 
continent  of  America,  to  form  the  vast  and  supposed 
gulf  of  Baffin's  Bay;  by  others,   to  be  one  large 
island ;  and  by  a  third  class,  to  be  a  cluster  of  islands 
intersected  by  a  variety  of  channels  running  from  sea 
to  sea,  but  so  blocked  up  with  ice  as  to  render  the 
passage  between  them  impracticable.    In  a  journal 
before  me  it  is  mentioned  that  a  strong  current  sets 
round  Cape  Farewell  to  the  Northwest,  and  that  the 
water  breaks  for  several  miles.    It  appears  probable, 
therefore,  from  this  circumstance,   that  Greenland 
does  not  consist  of  a  multitude  of  islands ;  because 
in  that  case  the  current  would  have  taken  its  direc- 
tion between  them,  instead  of  flowing  round  the  ex- 
tremity of  the  land.    The  junction  of  Greenland  with 
North  America  appears  to  me  to  be  likewise  impro- 
bable, from  the  following  reasons :  first,  that  Brown 
(as  already  mentioned)  never  saw  the  Western  land ;. 
next,  that  Heam  in  his  travels-  arrived  at  the  sea^ 
seals  having  been  seen  by  him:  and,  thirdly,  that 
Mackenzie,  whose  travels  lie  to  the  Westward  of 
Hearn's  course,  came  to  the  mouth  of  a  large  river, 
which  also  emptied  itself  into  the  Arctic  Ocean: 
and,  lastly,  from  the  great  probability  that  the  im- 
mense quantity  of  drift  wood  found  in  Baffin's  Bay, 
on  the  Coast  of  Labrador,  and  on   the  Nortutvest 
Coast  of  America,  has  been  deposited  there  after 


% 


<-k        ft 


» 


■^"i 


THfe  HORTR  POLE. 


Id? 


being  brought  down  by  Mackenzie's  River,   and 
driven  to  the  East  and  West,  wd  afterward  South- 
ward, according  to  the  direction  of  the  winds  and 
currents:  all  which  circumstances  combine,  in  my 
opinion,  to  furnish  a  ground  of  belief  that  North,  as 
well  as  South  America,  is  surrounded  by  the  ocean ; 
and  that  the  Northwest  Passage  is  to  be  sought  about 
latitude  72^    That  Greenland  is  an  island  seem^ 
also  to  be  highly  probable,  from  the  quantity  of  drift 
wood  found  on  the  Coast  of  Iceland ;  for  it  is  much 
more  natural  to  suppose  that  trunks  of  trees  found 
in  that  part  of  the  world  are  carried  off  from  the 
.  Northern  extremity  of  America,  and  driven  round 
the  North  of  Greenland,  than  that,  being  floated  from 
the  mouths  of  the  Obi,  Lena,  and  other  great  rivers 
of  Russia,  they  should  pass  Nova  Zembla,  round  the 
North  Cape,  to  the  prodigious  distance  of  20*  West 
longitude. 

Cape  Farewell,  the  Southern  extremity  of  Green- 
land, according  to  the  Requisite  Tabffs,  is  in  lati- 
tude 59"  38'  00"  North,  and  longitude  42*  42'  00"  West. 
By  observations  in  my  possession,  it  is  in  latitude 
59*  42'  North,  and  longitude  45*  16'  West. 


-* 


(..' 


THE  END. 


% 


^ 


